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  • English  (7,700)
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  • 1995-1999  (2,123)
  • 1980-1984  (2,164)
  • 1975-1979  (1,924)
  • 1965-1969  (1,502)
  • 1940-1944  (21)
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  • 1
    Monograph available for loan
    Monograph available for loan
    General climatology (1976)
    Warszawa : Polish Scient. Publ.
    Details Availability
    Call number: PIK N 456-11-0194
    Description / Table of Contents: Contents: 1. Climatology as a science ; 2. Climate-forming factors ; 3. Geographical distribution and variation of major meteorological elements ; 4. A brief survey of major types of climate ; 5. Changes and fluctuations of climates
    Type of Medium: Monograph available for loan
    Pages: XIV, 422 S. : graph. Darst., 1 Kt.
    Uniform Title: Klimatologia ogólna
    Language: English
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Carbonate rocks (1967)
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Details Availability
    Call number: 9/M 13.0083
    In: Developments in sedimentology
    Type of Medium: Monograph available for loan
    Pages: 471 S., Ill., graph. Darst., kt-.
    Series Statement: Developments in sedimentology 9A
    Language: English
    Location: Reading room
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  • 3
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    Publications on geodesy (1)
    Delft ; 1.1969-76.2010
    Details Availability
    Call number: S 90.0083
    ISSN: 0165-1706
    URL: http://www.ncg.knaw.nl/eng/publications/geodesy.html
    Language: English
    Branch Library: GFZ Library
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  • 4
    Series available for loan
    Series available for loan
    Detecting structural heat losses with mobile infrared thermography; Part III: Survey of USA CRREL (1975)
    Associated volumes
    Details Availability
    Call number: ZSP-202-348
    In: Detecting structural heat losses with mobile infrared thermography, Part III
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 348
    Description / Table of Contents: During the winter of 1973 - 74 a mobile infrared thermography system was used to survey the USA CRREL building at Hanover, New Hampshire. This report provides a description of excessive heat losses at several locations around the building. This report also discusses the need to carefully monitor meteorological conditions before starting a survey of a building exterior to determine if solar radiation decay from the building surface might interfere with thermographic analysis by masking the heat emanating from within the building.
    Type of Medium: Series available for loan
    Pages: ii, 9 S. : Ill.
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 348
    URL: http://hdl.handle.net/11681/5785
    Language: English
    Location: AWI Archive
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  • 5
    Series available for loan
    Series available for loan
    Biological aspects of terrestrial oil spills : USA CRREL oil research in Alaska, 1970-1974 ; [Final Report] (1975)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-202-346
    In: Research report / Cold Regions Research and Engineering Laboratory, 346
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - USA CRREL project and personnel involvement. - Part I. Introduction. - Background. - Literature review. - Part II. CRREL investigations from 1970 - 1974. - Initial literature survey (1970). - Oil detection kit development. - Survey of Cape Simpson, Alaska, natural crude oil seepages (1970). - Haines-Fairbanks military pipeline investigations (1971-1973). - Barrow investigations (1970-1974). - Fairbanks and Fox investigations. - Germination studies. - Physiological studies. - Dispersant studies. - Microbiological investigations. - Field investigations of accidental petroleum losses. - Part III. Recent related literature. - Part IV. Conclusions and recommendations. - USA CRREL reports, publications and presentations on Alaska oil spill research. - Literature cited.
    Description / Table of Contents: Knowledge concerning the biological effects of oil pollution on arctic and subarctic terrestrial ecosystems is limited. USA CRREL research personnel conducted investigations from 1970 through 1974 to expand information in this field. Objectives were to: 1) define the ecosystems most sensitive to the presence of crude oil or its refined products, 2) quantify and understand the injury response, and 3) establish time frames for manifestation of damage and natural restorative processes in arctic and subarctic regions. This was accomplished through: 1) surveys of natural oil seepages and past accidential spills in the Arctic and Subarctic, 2) initiation of controlled oil spills and 3) detailed laboratory investigations. Results demonstrated that terrestrial oil spills will to some degree be detrimental to both arctic and subarctic plant communities. Degree and longevity of damage will be influenced primarily by the magnitude of the spill, season of occurrence and existing soil moisture content. Rapid recovery of plant communities subjected to spills will occur only if root systems remain relatively unaffected. Damage will be more extensive and long-term when root systems are saturated with oil. Effects of damage will be manifested gradually over several seasons being influenced by winter stresses. Variation does exist in plant species susceptibility. Carex aquatilis, a predominant sedge of the arctic, is markedly resistant to crude oil damage. In the taiga Picea mariana is very susceptible. Plant recovery can be enhanced through the application of fertilizer. Fertilization, in addition to its direct effect on plant nutrition, will stimulate microbial decomposition of crude oil.
    Type of Medium: Series available for loan
    Pages: vii, 66 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 346
    URL: https://apps.dtic.mil/docs/citations/ADA047365
    Language: English
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  • 6
    Series available for loan
    Series available for loan
    Seasonal variations of chemical constituents in annual layers of Greenland deep ice deposits (1975)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-202-347
    In: Research report / Cold Regions Research and Engineering Laboratory, 347
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Experimental. - Results and discussion. - Applications. - Literature cited.
    Description / Table of Contents: Chemical analysis of century-old ice from continuous 5 to 7 year intervals of three ice cores from south and central Greenland (Dye 3, Milcent and Crete) show maximum concentrations of Na, Mg,Ca, K, and Al during early spring and minimum concentrations during late summer and early fall. Peak spring values are as much as 10 times greater than fall values. Because of the large seasonal chemical variations, samples used for depth-age or annual deposition rate studies must represent accumulation from exactly one year or whole multiples of a year. The seasonal chemical variations seem promising as a new method of defining annual layers and thus dating old ice cores.
    Type of Medium: Series available for loan
    Pages: iii, 5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 347
    URL: https://apps.dtic.mil/docs/citations/ADA021319
    Language: English
    Location: AWI Archive
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  • 7
    Series available for loan
    Series available for loan
    Attenuation of visible light by falling snow (1969)
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-202-242
    In: Research report, 242
    Description / Table of Contents: The attenuation of visible light by falling snow was studied by making simultaneous attenuation measurements and snow concentration measurements. The attenuation coefficient was calculated from photometric measurements and from visual observations. Snow concentration in the air was evaluated by two methods: from Formvar replicas collected during the snowfall, and by mass accumulation of snow in collecting pans. The snowflakes were arbitrarily classified by crystal types according to their estimated fall velocity. It was found that the correlation between extinction coefficient (attenuation) and snow concentration was generally much higher by types than when all snowflakes were considered together regardless of crystal components and degree of riming. Two types, apparently improperly classified, displayed lower correlations than the overall group. When no fog is present during the snowfall, the experimental results coincide well with attenuation theory if a reasonable correction is applied to the values obtained in the measurement of snowflake diameters. Measurements of mass flux indicate that for a given intensity the attenuation caused by snow is an order of magnitude greater than that caused by the same mass flux of rain.
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 242
    URL: https://hdl.handle.net/11681/5949
    Language: English
    Note: CONTENTS: Preface. - Abstract. - Introduction. - Initial theoretical considerations. - Light attenuation by particles. - Basis of attenuation meter measurements. - Contrast reduction and visual range. - Transmissometer theory, Pritchard photometric method. - Terminal velocity of snowflakes. - Methods of measurement: Light attenuation. - Duntley (Scripps Institution) attenuation meter. - "Meteorological range" observations. - Pritchard photometric method. - Methods of measurement: Atmospheric concentration of snowflakes. - Replication method. - Mass accumulation method. - Analysis of snow samples. - Terminal velocity of snowflakes. - Flux density and atmospheric concentration. - Mass accumulation rate. - Concurrent attenuation due to fog. - Discussion of results. - Computational methods. - Correlations: Attenuation coefficient vs area concentration. - Correlations: Attenuation coefficient vs are a flux. - Correlations: Attenuation coefficient vs mass concentration and mass flux. - Comparison of sampling methods for mass flux. - Attenuation of visible light by snow compared to rain. - Literature cited. - Appendix A.
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  • 8
    Series available for loan
    Series available for loan
    Interpretation of young ice forms in the Gulf of St. Lawrence using side-looking airborne radar and infrared imagery (1975)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-202-337
    In: Research report
    Description / Table of Contents: Contents: Introduction. - Surface ice observations. - Imagery interpretation. - Side-looking airborne radar. - Infrared. - Conclusions. - Literature cited.
    Description / Table of Contents: Ice conditions during mid-January 1974 in the Gulf of St. Lawrence and in the estuaty as far upstream as Rimouski are described utilitizing side-looking airborne radar, infrared and photographic imagery. The interpretations were verified by simultaneous surface observations on the ice by investigators operating from the CSS Dawson. The ice examined was undergoing rapid drift and deformation and showed a wide variety of thin ice (0-40 cm) features formed under the influence of strong winds and currents. These observations should serve as a guide in interpreting ice conditions in similar areas where ground truth data are not available.
    Type of Medium: Series available for loan
    Pages: 41 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 337
    URL: http://www.worldcat.org/oclc/2327064
    Language: English
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  • 9
    Series available for loan
    Series available for loan
    The bearing capacity of floating ice plates subjected to static or quasi-static loads : a critical survey (1975)
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-202-333
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Introduction. - Analogy method. - Method based on the bending theory of elastic plates and the criterion [Sigma]max = [Sigma]f. - Methods based on viscoelastic theories. - Methods based on the yield line theory or limit analysis. - Comparison of analytical and test results. - General remarks. - Effect of bending and shearing forces on deflection of an ice cover. - Determination of Pf(O). - Determination of Pf(t). - Determination of [Sigma]f. - Summary and recommendations. - Literature cited.
    Description / Table of Contents: This report contains a critical survey of the literature on the bearing capacity of floating ice plates. It consists of a discussion of general questions, a critical survey of analytical attempts to determine the bearing capacity of floating ice plates, and a survey of field and laboratory tests on floating ice plates and their relation to the analytical results. The paper concludes with a systematic summary of the results, a discussion of observed shortcomings, and suggestions for needed investigations.
    Type of Medium: Series available for loan
    Pages: iv, 43 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 333
    URL: http://www.worldcat.org/oclc/1387849
    Language: English
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  • 10
    Series available for loan
    Series available for loan
    Electrolytic conductivity of snow and glacier ice from Antarctica and Greenland (1968)
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-202-248
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Analytical procedures. - Results and discussion. - Literature cited.
    Description / Table of Contents: Conductivity measurements have been made on snow and ice samples from pits and deep drillholes at a number of localities in Antarctica and Greenland. Conductivities of the order 1-2 [My]mho/cm only were recorded at the inland sites. Data from deep cores representing more than 1900 years of continuous snow accumulation at Byrd Station, Antarctica, and more than 400 years deposition at Inge Lehmann, Greenland, showed no significant variations of conductivity with time. Measurements of freshly precipitated snow from a single coastal location in McMurdo Sound, Antarctica, also yielded relatively low conductivities of the order 3-4 [My]mho/cm. The substantial increase observed in the conductivity of core samples from near the surface of the Ross Ice Shelf at Little America V can be attributed most probably to windborne salts of marine origin that had accumulated on the surface after the snow was deposited. A peak conductivity of 49 [My]mho/cm was recorded in snow estimated to have been deposited within 20 km of the seaward edge of the Ross Ice Shelf and the maritime effect could still be detected in samples deposited more than 40 km from the ice front. For samples deposited at distances of greater than 200 km from the edge of the Ross Ice Shelf conductivities never exceeded 2 [My]mho/cm. The very low conductivities observed in ice cores from near the bottom of the Ross Ice Shelf confirm earlier conclusions based on detailed petrographic studies oi the cores that the 258-m-thick ice shelf at Little America V is composed entirely of glacial ice.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 248
    URL: https://dx.doi.org/10.1029/JB073i012p03643
    Language: English
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  • 11
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    International project on paleolimnology and late cenozoic climate (1979)
    Innsbruck : Univ.-Verl. Wagner ; Nachgewiesen 2.1979 -
    Details Availability
    Call number: ZSP-387
    Language: English
    Branch Library: GFZ Library
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  • 12
    Monograph available for loan
    Monograph available for loan
    Guidelines for seismic microzonation studies (1995)
    St-Rémy-lès-Chevreuse : Association Francaise du Genie Parasismique
    Details Availability
    Call number: M 15.0048
    Type of Medium: Monograph available for loan
    Pages: Getr. Zähl. : graph. Darst, Kt.
    Uniform Title: Guide méthodologique pour la réalisation d'études de microzonage sismique
    Language: English
    Location: Upper compact magazine
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  • 13
    Series available for loan
    Series available for loan
    Stability of difference approximation to shock wave propagation in inhomogeneous elastic-plastic media (1969)
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
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    Call number: ZSP-202-277
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Nomenclature. - Introduction. - Basic equations. - Constitutive relations. - Elastic region. - Plastic region. - Stability of the differential equation. - Stability of the difference equation. - Literature cited.
    Description / Table of Contents: An analysis is made of the stability of difference approximation to one-dimensional shock wave propagation in elastic-plastic media. The necessary condition for stability is obtained.
    Type of Medium: Series available for loan
    Pages: iv, 9 Seiten
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 277
    URL: http://www.worldcat.org/oclc/5974046
    Language: English
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  • 14
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    Bulletin / Geological Survey of Finland (326)
    Helsinki [u.a.] ; 326.1984 -
    Details Availability
    Call number: Z 92.0098
    ISSN: 0367-522X
    Former Title: Bulletin / Geologinen Tutkimuslaitos
    Language: English
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  • 15
    Series available for loan
    Series available for loan
    Diffusion law for the dispersion of hard particles in an ice matrix that undergoes simple shear deformation (1968)
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
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    Call number: ZSP-202-252
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Discussion. - Conclusion. - Literature cited.
    Description / Table of Contents: A diffusion equation is obtained that describes the mechanical dispersion of a dilute mixture of solid particles within an ice matrix that is undergoing deformation. It is shown that within the limits of time intervals and strain rates appropriate to the movement of glaciers and ice sheets the dispersal distance usually is no larger than a distance about one order of magnitude greater than the size of the particles themselves.
    Type of Medium: Series available for loan
    Pages: iv, 6 Seiten , Illistrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 252
    URL: http://dx.doi.org/10.3189/S0022143000030963
    Language: English
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  • 16
    Series available for loan
    Series available for loan
    Bubble coalescence in ice as a tool for the study of its deformation history (1968)
    Hanover, NH : U.S. Army Materiel Command Cold Regions Research & Engineering Laboratory
    Associated volumes
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    Call number: ZSP-202-251
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Application to ice sheets and ice shelves. - Summary. - Literature cited.
    Description / Table of Contents: An analysis is made of the rate of bubble coalescence in a deforming ice mass. A total strain of at least 8 is required before appreciable coalescence occurs, The analysis has.been applied to deforming ice shelves and ice sheets. No appreciable coalescence is expected in ice shelves but coalescence should occur in ice sheets (or glaciers) if the shear strain rate at the bottom surface is of the order of 0.075/yr or larger. Measurements of bubble concentration are capable of setting limits on paleo-strain rates of the present ice sheets. Bubble migration down temperature gradients presents complications to the study of bubble coalescence.
    Type of Medium: Series available for loan
    Pages: iv, 5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 251
    URL: https://dx.doi.org/10.3189/S0022143000030951
    Language: English
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  • 17
    Series available for loan
    Series available for loan
    Comparison between measured and theoretical temperature profiles of the Camp Century, Greenland, borehole (1968)
    Hanover, NH : U.S. Army Materiel Command, Cold Regions Research & Engineering Laboratory
    Associated volumes
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    Call number: ZSP-202-246
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Summary. - Introduction. - Theory. - Discussion. - Literature cited.
    Description / Table of Contents: Steady-state temperature profiles are calculated for the borehole drilled through the Greenland ice sheet at Camp Century. The profiles are found by modifying Robin's theory through the addition of several correction terms. One of these terms is the internal heating arising from creep deformation. The importance of this term was emphasized by Lliboutry. The new theoretical profiles do not differ appreciably from the profile derived from Robin's theory. The theoretical profiles do differ substantially from the Camp Century profile measured by Hansen. It is concluded that Hansen's observations are evidence that factors such as accumulation rate and the upper surface temperature are not in a long-term steady-state condition. Better agreement between theoretical and measured curves is obtained if it is assumed that the accumulation rate was about 40% smaller in the past and that the mean annual surface temperature varied by about 0.5°C over the past 1000 years.
    Type of Medium: Series available for loan
    Pages: iv, 13 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 246
    URL: https://dx.doi.org/10.1029/JB073i008p02691
    Language: English
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  • 18
    Series available for loan
    Series available for loan
    Exchange adsorption of strontium on clay minerals (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1140-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, C-26 S.
    Series Statement: U.S. Geological Survey bulletin 1140-C
    Language: English
    Location: Lower compact magazine
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  • 19
    Series available for loan
    Series available for loan
    Terrestrial impact structures - a bibliography 1965 - 68 (1969)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1320)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 39 S.
    Series Statement: U.S. Geological Survey bulletin 1320
    Language: English
    Location: Lower compact magazine
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  • 20
    Series available for loan
    Series available for loan
    Gold in the Black Pine mining district, southeast Cassia County, Idaho (1984)
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
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    Call number: SR 90.0001(1382-E)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, E-15 S.
    Series Statement: U.S. Geological Survey bulletin 1382-E
    Language: English
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  • 21
    Series available for loan
    Series available for loan
    Upper Pleistocene pyroclastic-flow deposits and lahars south of Mount St. Helens volcano, Washington (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1383-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, B-20 S.
    Series Statement: U.S. Geological Survey bulletin 1383-B
    Language: English
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  • 22
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    Series available for loan
    Mineral resources of the San Pedro Parks Wilderness and vicinity, Rio Arriba and Sandoval Counties, New Mexico (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1385-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, C-29 S. + 12 pl.
    Series Statement: U.S. Geological Survey bulletin 1385-C
    Language: English
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  • 23
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    Mineral resources of the Eagle Cap Wilderness and adjacent areas, Oregon (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1385-E)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IX, E-100 S. + 1 pl.
    Series Statement: U.S.Geological Survey bulletin 1385-E
    Language: English
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  • 24
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    Mineral resources of the South Warner Wilderness, Modoc County, Californien (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1385-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, D-31 S. + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 1385-D
    Language: English
    Location: Lower compact magazine
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  • 25
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    Yeoloyikó chártis tís Elládhas 1:500 000 (1983)
    Stuttgart : Institute of Geology and Mineral Exploration
    Details Availability
    Call number: K 97.0014/1-2
    Pages: total 140x192, gef. cm
    Edition: 2nd ed.
    Language: English
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  • 26
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    Series available for loan
    Marine trace fossils in the upper Jurassic Bluff Sandstone, southeastern Utah (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1395-I)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, I-12 S.
    Series Statement: U.S. Geological Survey bulletin 1395-I
    Language: English
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  • 27
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    The geologic story of Arches National Park (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1393)
    In: U.S. Geological Survey bulletin
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    Pages: IX, 113 S.
    Series Statement: U.S. Geological Survey bulletin 1393
    Language: English
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  • 28
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    Mineral resources of the Teton Corridor, Teton County, Wyoming (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1397-A)
    In: U.S. Geological Survey bulletin
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    Pages: VI, A-51 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1397-A
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  • 29
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    Recent landslides in Alameda County, California (1940-71) : an estimate of economic losses and correlations with slope, rainfall, and ancient landslide deposits (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1398)
    In: U.S. Geological Survey bulletin
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    Pages: III, 21 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1398
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  • 30
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    Mineral resources of the Gila Primitive Area and Gila Wilderness, New Mexico (1979)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1451)
    In: U.S. Geological Survey bulletin
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    Pages: XII, 229 S. + 4 pl.
    Series Statement: U.S. Geological Survey bulletin 1451
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  • 31
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    Directory to U.S. Geological Survey program activities in coastal areas 1974-76 (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1428)
    In: U.S. Geological Survey bulletin
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    Pages: IV, 154 S.
    Series Statement: U.S. Geological Survey bulletin 1428
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  • 32
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    Geology and mineral resources of the Kuluncak-Sofular area (Malatya K-39a1 and K39-a2 quadrangles), Turkey (1978)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1429)
    In: U.S. Geological Survey bulletin
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    Pages: IV, 58 S. + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 1429
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  • 33
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    Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar (10 5 pascals) pressure and at higher temperatures (1978)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1452)
    In: U.S. Geological Survey bulletin
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    Pages: III, 456 S.
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  • 34
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    Geology of the Hot Springs quadrangle Fall River and Custer Counties, South Dakota (1967)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1063-K)
    In: U.S. Geological Survey bulletin
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    Pages: IV S., S. 427-442 + 1 pl.
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  • 35
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    The Reinhardt Thiessen coal thin-section slide collection of the U.S. Geological Survey : catalog and notes (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1432)
    In: U.S. Geological Survey bulletin
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    Pages: IV, 58 S.
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  • 36
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    Mineral resources of the White Mountain Wilderness and adjacent areas, Lincoln County, New Mexico (1979)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1453)
    In: U.S. Geological Survey bulletin
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    Pages: VII, 135 S. + 2 pl.
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  • 37
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    Phosphate investigation in Florida 1934 and 1935 (1941)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(906-F)
    In: U.S. Geological Survey bulletin
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    Pages: IV S., S. 267-345, VI S.
    Series Statement: U.S. Geological Survey bulletin 906-F
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  • 38
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    Neogene stratigraphy and paleontology of southern Almería Province, Spain : an overview (1978)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1454)
    In: U.S. Geological Survey bulletin
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    Pages: IV, 49 S.
    Series Statement: U.S. Geological Survey bulletin 1454
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  • 39
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    Triassic stratigraphy in the northern part of the Culpeper basin, Virginia and Maryland (1977)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1422-C)
    In: U.S. Geological Survey bulletin
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    Pages: III, C-17 S. + 1 pl.
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  • 40
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    Eocene rocks in northeast Washington : radiometric ages and correlation (1977)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1433)
    In: U.S. Geological Survey bulletin
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    Pages: IV, 41 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1433
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  • 41
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    Climatic implications of two pollen analyses from newly recognized rocks of latest Pliocene age in the Washburn Range, Yellowstone National Park, Wyoming (1978)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1455)
    In: U.S. Geological Survey bulletin
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    Pages: III, 13 S.
    Series Statement: U.S. Geological Survey bulletin 1455
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  • 42
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    Mount Belknap and Red Hills calderas and associated rocks, Marysvale volcanic field, west-central Utah (1979)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1468)
    In: U.S. Geological Survey bulletin
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    Pages: III, 34 S.
    Series Statement: U.S. Geological Survey bulletin 1468
    Language: English
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  • 43
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    Differential sea ice drift (1975)
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory,
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    Call number: ZSP-202-329
    In: Research report
    Description / Table of Contents: CONTENTS: General Introduction. - Part I. Spatial and temporal variations in sea ice deformatfon. - Introduction. - Approach. - Site location and data collection procedures. - Data analysis. - Strain results. - Comparison of mesoscale deformation with macroscale deformation. - Nature of the ice pack rotation. - Conciusion. - Literature cited. - Part Il. Comparison of mesoscale strain measurements with linear drift theory predictions. - Introduction. - List of symbols. - Linear drift equations. - Ice drift solutions. - Comparison of theory with mesoscale measurements. - A more general linear constitutive law. - Conclusions. - Literature cited. - Appendix Relative magnitudes of differential drift forces. - Abstract.
    Description / Table of Contents: Measurements of mesoscale sea ice deformation over a region approximately 20 km in diameter were made over a five-week period in the spring of 1972 at the main AIDJEX camp in the Beaufort Sea. They have been analyzed to determine nonlinearities in the ice velocity field (due to the discrete small-scale nature of the ice pack), as well as a continuum mode of deformation represented by a least squares strain rate tensor and vorticity. The deformation rate time series between Julian day 88 and 113 exhibited net areal changes as large as 3% and deformation rates up to 0.16% per hour. In the principal axis coordinate system, the strain rate typically exhibited a much larger compression (or extension) along one axis than along the other. Persistent cycles at ~12-hour wavelengths were observed in the divergence rate. A comparison of the average residual error with the average strain rate magnitude indicated that strains measured on a scale of 10 km or greater can serve as a valid measure of the continuum motion of the sea ice. This conclusion is also substantiated by a comparison between the mesoscale deformation, and macroscale deformation measured over a ~100-km-diameter region. Vorticity calculations indicate that at low temporal frequencies ( 〈 0.04 hr^-1 ) the whole mesoscale array rotates essentially as an entity and consequently the low frequency vorticity can accurately be estimated from the rotation of a single floe. (Part I) A comparison of mesoscale strain measurements with the atmospheric pressure field and the wind velocity field indicated that the ice divergence rate and vorticity followed the local pressure and wind divergence with significant correlation. For low atmospheric pressures and converging winds, the divergence rate was negative with the vorticity being counterclockwise. The inverse behavior was observed for high pressures and diverging winds. This behavior agreed with predictions based upon the infinite boundary solution of a linearized drift theory in the absence of gradient current effects and using the constitutive law proposed by Glen for pack ice. The best least squares values of the constitutive law parameters [Eta] and [Zeta] were found to be given by ~10^12 kg sec^-1. Using typical divergence rates, these values yielded compressive stresses of the magnitude of 10^5 N m^-1, which are similar to values suggested by the Parmerter and Coon ridge model. In general, the infinite boundary solution of the linear drift equation indicates that in a low pressure region that is reasonably localized in space, the ice would be expected to converge for high compactness (winter) and diverge for low compactness (summer). Calculations were also carried out using a more general linear viscoelastic constitutive law that includes memory effects and that includes a generalized Hooke's law as well as the Glen law as special cases. A best fit of this more general calculation with strain measurements indicates, overall, a better agreement with viscous behavior than with elastic behavior, with the frequency behavior of the estimated "viscosities" similar to the Glen law behavior at temporal frequencies less than ~0.01 hr^-1 (Part II)
    Type of Medium: Series available for loan
    Pages: v, 37 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 329
    URL: http://www.worldcat.org/oclc/1387886
    Language: English
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  • 44
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    A digital computer simulation of the annual snow and soil thermal regimes at Barrow, Alaska (1975)
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-331
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Introduction. - An overview of the model structure and operation. - Operation of subroutines. - TSTART. - FOMO. - REAWEA. - SEARCH. - STEMP. - TUNPIC. - Development history of the simulator. - The simulation of snow fence effects. - Urbanization and meltout. - Conclusion. - Literature cited. - Appendix A: Mathematical notation. - Appendix B: Computerprogram. - Abstract.
    Description / Table of Contents: An annual snow-soil simulator for Arctic tundra was developed using coupled models of surface equilibrium temperature and substrate thermal diffusion. Snow ripening, melt and accumulation are modeled in the simulator which is forced with daily weather data. The simulator predicts that a snow fence array capable of producing drift deeper than 4.2 meters will initiate a permanent snowfield at Barrow, Alaska. Such a man-induced snowfield could serve as a reliable source of fresh water for Barrow and similar villages in the North Slope region of Alaska. Further analysis indicated that albedo reduction due to dust fall, snow removal, etc., is dominant over aerodynamic effects in producing the early spring meltout observed at Barrow Village.
    Type of Medium: Series available for loan
    Pages: iv, 18 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 331
    URL: http://www.worldcat.org/oclc/1381484
    Language: English
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  • 45
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    Strain rate effect on the strength of frozen silt (1975)
    Hanover, N.H. : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-350
    In: Research report / Cold Regions Research and Engineering Laboratory, 350
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 350
    URL: https://usace.contentdm.oclc.org/digital/collection/p266001coll1/id/6211
    Language: English
    Note: CONTENTS: Abstract. - Preface. - Introduction. - Sample preparation. - Apparatus and testing procedure. - Test results. - Uniaxial strength. - Initial tangent and 50% strength moduli. - Specific energy. - Discussion. - Testing method. - Compressive strength. - Tensile strength. - Ductile and brittle fracture.. - Initial tangent and 50% stress moduli. - Specific energy. - Conclusions and recommendations. - References. - Appendix A: Description of soil and calculations. - Appendix B: Description of the LVDT and averaging circuits. - Appendix C: Determination of strain in the neck section of a dumbbell specimen.
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  • 46
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    Microspherules in snow and ice-fog crystals (1969)
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
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    Call number: ZSP-202-245
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Snow crystals in Greenland. - Microspherules. - Microspherules in snow and ice-fog crystals. - Concentration and radii of spherules. - Discussion and conclusions. - Literature cited.
    Description / Table of Contents: Spherules found in snow crystals, ice-fog crystals, fallout particles, and fly ash were studied with an electron microscope using the electron diffraction method. The central part of the residues of 1004 specimens of natural snow crystals from Greenland, the United States, and Japan were examined; 14 spherules 0.1 to 1.5? in radius were found among them. The residues of 658 artificial ice-fog crystals formed from water vapor in flue gases of coal-burning electric power plants at Fairbanks, Alaska, were also examined; nine spherules were found. Spherules similar to those found in ice-fog residues were found in furnace-produced fly ash fallout at Fairbanks, Alaska. Electron and optical microscope examination of spherules found in Greenland snow reveals a size distribution of the form dN/d(log r) = Cr-ß where ß approximately 3. The properties of spherules and the mean mass of snow crystals from Greenland are described. The electron microscope study indicated that less than 0.7% of the 1004 snow crystals contained spherules of possible extraterrestrial origin, and that snow crystals are formed mainly on clay mineral particles by heterogeneous nucleation.
    Type of Medium: Series available for loan
    Pages: iv, 10 Seite , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 245
    URL: https://apps.dtic.mil/sti/citations/tr/AD0691326
    Language: English
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  • 47
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    Some physical properties of alpine snow (1969)
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research & Engineering Laboratory
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    Call number: ZSP-202-271
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Previous work. - Conduct of the research. - Fundamental properties of snow. - Derived properties of snow. - Environmental effects. - Conclusions. - Literature cited. - Abstract.
    Description / Table of Contents: One of the great deficiencies in snow science is the lack of an analytical framework for much of the snow cycle. Snow research to date has largely consisted of measuring index properties of snow, such as bulk density and snow strength, and correlating them. This is useful, particularly for engineering purposes, but it does not grapple with the basic problem of what fundamental properties of snow determine the magnitude of the index properties and how these properties respond to environmental conditions. This study was an attempt to measure, quantitatively, the fundamental properties of grain size, shape, and fabric (relationship between grains) and relate these to the index or derived properties of bulk density, shear and tensile strength, permeability for air, and the dielectric static permittivity and loss tangent. Despite numerous difficulties in defining fabric and quantifying it, it was possible to show that: 1) snow strength is a function of bond area with a relationship in the low density range that is described by: [Sigma]f = [Sigma]i exp - (0.14nf) where [Sigma]f is failure strength, [Sigma]i is the final strength of ice, and nf is the porosity on the failure surface; and 2) the rate of densification of low density snow can be explained in part by high stress concentrations (on the order of 10^7 dynes /cm^2) at intergranular contacts and by such factors as riming on crystals. The effect of the environmental factors of time, temperature, and gravitational stress is difficult to study in situ because they are not independent variables. However, it appears that their study is simplified when we study the fundamental properties of snow as opposed to index properties.
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    Pages: v, 70 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 271
    URL: http://www.worldcat.org/oclc/5325802
    Language: English
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  • 48
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    Thermal instability in a layer of water formed by melting ice from below (1969)
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
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    Call number: ZSP-202-263
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theoretical background. - Experimental apparatus and procedures. - Results and discussion. - Conclusions. - Literature cited.
    Description / Table of Contents: The transition in the mode of heat transfer from conduction to convection in a layer of water formed continuously by melting ice from below has been determined experimentally. This was accomplished by locating the inflection point on the curve relating the water-ice interface (or melting front) and time. Thus, the critical Rayleigh number, Rac, at which convective heat transfer started can be correlated empirically as a function of warm plate temperature, Ts, by Rac= 14,200 exp(-6.64 x 10^-2 Ts). This relation is valid for Ts varying from 7.72 to 25.50°C. The initial ice temperature T0 was varied from -4.8 to -22.00°C. The effect of T0 was found to be insignificant. Homogeneous, bubble-free ice was prepared and used in all the experiments.
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    Pages: iv, 12 Seiten , Illustrations
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 263
    URL: http://www.worldcat.org/oclc/5325820
    Language: English
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  • 49
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    On plates sealing an incompressible liquid (1968)
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
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    Call number: ZSP-202-260
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction and statermnt of problem. - Solution of problem shown in Figure 3. - Solution of problem shown in Figure 4. - The negligibility of the effects of buoyancy and incompressibility of the sealed liquid. - Literature cited.
    Description / Table of Contents: After a brief description of the circumstances which led to the investigation of the title problem and discussion of some related previous investigations, exact solutions are derived for a circular plate which seals an incompressible liquid, is clamped along the boundary and is subjected at an arbitrary point to a lateral concentrated force P. For the case when the plate is covered by a thin liquid layer the solution is obtained in closed form. When this liquid layer is absent, the solution is obtained as an infinite series. The paper concludes with a study of the range of the parameter ([Lambda] a) for which the effort of buoyancy is negligible upon the deflections and stresses in the plate.
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    Pages: iv, 11 Seiten , Illustartionen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 260
    URL: http://www.worldcat.org/oclc/5325791
    Language: English
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  • 50
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    Bubbles and bubble pressures in Antarctic glacier ice (1968)
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
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    Call number: ZSP-202-249
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Analytical procedures. - Results and discussion. - Bubbles in ice. - Conclusions. - Literature cited.
    Description / Table of Contents: Application of the gas law to fourth-place density measurements of ice samples from two deep drill holes at Byrd Station and Little America V, Antarctica, shows that virtually all density increase beyond the pore close-off density (0.830 g/cm^3) can be attributed to compression of the entrapped bubbles of air. Data from Byrd Station also indicate that the lag between overburden pressure and bubble pressure, initially 4-5 kg/cm^2 at pore close-off, diminishes to less than 1.0 kg/cm^2 at about 200-m depth. By substituting the overburden pressure for the bubble pressure in the pressure-density relationship based on the gas law, ice densities below 200 m can be calculated more accurately than they can be measured per se on cores because of the relaxation that occurs in samples recovered from high confining pressures. This relaxation, resulting in a progressive increase in the bulk volume of the ice with time, is generally attributed to decompression of the entrapped air bubbles following removal of the ice from high confining pressures. However, calculations of the stress in ice due to bubble pressure, together with measurements of bubble sizes in cores from various depths at Byrd Station, both tend to indicate that there has'been negligible decompression of the inclosed bubbles. It is suggested that most of this relaxation may be due to the formation of microcracks in the ice. Anomalous bubble pressure-density relations at Little America V tend to confirm abundant stratigraphic evidence of the existence of considerable deformation in the upper part of the Ross Ice Shelf. Studies of crystal-bubble relations at Byrd Station revealed that the concentration of bubbles in ice remains remarkably constant at approximately 220 bubbles per cm^3. Bubbles and crystals were found to be present in approximately equal numbers at pore close-off at 64-m depth, at which level the average bubble diameter was 0.95 mm, decreasing to 0.49 mm at 116 m and to 0.33 mm at 279 m. Despite a tenfold increase in the size of crystals between 64 and 279 m, the bubbles showed no tendency to migrate to grain boundaries during recrystallization of the ice. The observation that most of the bubbles had assumed substantially spherical shapes by 120-m depth points to essentially hydrostatic conditions in the upper layers of the ice sheet at Byrd Station.
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    Pages: iv, 16 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 249
    URL: https://www.worldcat.org/de/title/6023806
    Language: English
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  • 51
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    Unknown
    Sedimentary provinces of the world : hydrocarbon productive and nonproductive 1:50 000 000 (1984)
    Tulsa, Oklahoma : American Association of Petroleum Geologists
    Details Availability
    Call number: K 93.0012
    Pages: Erl.
    Language: English
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  • 52
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    Chromite deposits in the Seiad Valley and Scott Bar quadrangles, Siskiyou County, California (1981)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1382-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, D-17 S.
    Series Statement: U.S. Geological Survey bulletin 1382-D
    Language: English
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  • 53
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    Influence of rainfall and ancient landslide deposits on recent landslides (1950-71) in urban areas of Contra Costa County, California (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1388)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, 18 S. + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 1388
    Language: English
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  • 54
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    Aeromagnetic and limited gravity studies and generalized geology of the Bodie Hills region, Nevada and California (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1384)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 38 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1384
    Language: English
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  • 55
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    The Supai Group : subdivision and nomenclature (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1395-J)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, J-11 S.
    Series Statement: U.S. Geological Survey bulletin 1395-J
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  • 56
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    Changes in stratigraphic nomenclature by the U.S. Geological Survey, 1973 (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1395-A)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, A-68 S.
    Series Statement: U.S. Geological Survey bulletin 1395-A
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  • 57
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    Mineral resources of the Beartooth Primitive Area and vicinity, Carbon, Park, Stillwater, and Sweet Grass Counties, Montana, and Park County, Wyoming. (1979)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1391-F)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VIII, F-125 S. + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 1391-F
    Language: English
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  • 58
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    Mineral resources of the Laramie Peak study area, Albany and Converse Counties, Wyoming (1977)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1397-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, B-35 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1397-B
    Language: English
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  • 59
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    A summary of Tertiary volcanic stratigraphy of the southwestern High Plateaus and adjacent Great Basin, Utah (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1405-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, B-20 S.
    Series Statement: U.S. Geological Survey bulletin 1405-B
    Language: English
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  • 60
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    Geology of the Rockland and Arbon quadrangles, Power County, Idaho (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1399)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VII, 115 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1399
    Language: English
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  • 61
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    Geology of the Precambrian W (lower Precambrian) rocks in western Gogebic County, Michigan (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1407)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, 40 S + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1407
    Language: English
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  • 62
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    Subsurface structure in part of southwestern New York and mode of gas in the Medina group; Pt. 2. (1941)
    Associated volumes
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    Call number: SR. 90.0001(899-B)
    In: U.S. Geological Survey bulletin
    In: Geologic structure and occurrence of gas in part of southwestern New York
    Type of Medium: Series available for loan
    Pages: III S., S. 69-93, III S.
    Series Statement: 899-B
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  • 63
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    Series available for loan
    Mineral resources of the Jarbidge Wilderness and adjacent areas, Elko County, Nevada (1977)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1439)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VII, 79 S. + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 1439
    Language: English
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  • 64
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    Paleozoic and Mesozoic stratigraphy of the northern part of the Ruby Range, southwestern Montana (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1405-I)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, I-26 S.
    Series Statement: U.S. Geological Survey bulletin 1405-I
    Language: English
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  • 65
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    A gravity study of the northern part of the Arctic National Wildlife Range, Alaska (1978)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1440)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, 21 S. + 3 pl.
    Series Statement: U.S. Geological Survey bulletin 1440
    Language: English
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  • 66
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    Series available for loan
    Rapid analysis of silicate, carbonate, and phosphate rocks : revised edition (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1401)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, 76 S.
    Series Statement: U.S. Geological Survey bulletin 1401
    Language: English
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  • 67
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    New and refined methods of trace analysis useful in geochemical exploration (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1408)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 105 S.
    Series Statement: U.S. Geological Survey bulletin 1408
    Language: English
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  • 68
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    Mineral resources of the La Garita Wilderness, San Juan Mountains, southwestern Colorado (1977)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1420)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, 65 S. + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 1420
    Language: English
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  • 69
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    Bedrock geology of the Conconully quadrangle, Okanogan County, Washington (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1402)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 58 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1402
    Language: English
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  • 70
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    Geology of the Juazohn quadrangle, Liberia (1978)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1448)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 31 S.
    Series Statement: U.S. Geological Survey bulletin 1448
    Language: English
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  • 71
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    Series available for loan
    Latin America's petroleum prospects in the energy crisis (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1411)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 40 S.
    Series Statement: U.S. Geological Survey bulletin 1411
    Language: English
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  • 72
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    Series available for loan
    Feasibility and cost of using a computer to prepare landslide susceptibility maps of the San Francisco Bay Region, California (1978)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1443)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, 27 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1443
    Language: English
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  • 73
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    Series available for loan
    The Colombia River Basalt Group in the Spokane quadrangle, Washington, Idaho, and Montana (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1413)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 39 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1413
    Language: English
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  • 74
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    Series available for loan
    A manual on fire assaying and determination of the noble metals in geological materials (1977)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1445)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, 58 S.
    Series Statement: U.S. Geological Survey bulletin 1445
    Language: English
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  • 75
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    Series available for loan
    Physical properties of the coexisting phases and thermochemical properties of the H 2 O componet in boiling NaCl solutions (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1421-A)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, A-73 S.
    Series Statement: U.S. Geological Survey bulletin 1421-A
    Language: English
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  • 76
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    Series available for loan
    The volumetric properties of aqueous sodium chloride solutions from 0¹ to 500¹ C at pressures up to 2000 bars based on a regression of available data in the literature (1977)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1421-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, C-36 S.
    Series Statement: U.S. Geological Survey bulletin 1421-C
    Language: English
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  • 77
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    Eocene fluvial drainage patterns and their implications for uranium and hydrocarbon exploration in the Wind River Basin, Wyoming (1978)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1446)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, 21 S.
    Series Statement: U.S. Geological Survey bulletin 1446
    Language: English
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  • 78
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    Series available for loan
    Thermodynamic properties of the coexisting phases and thermochemical properties of the NaCl component in boiling NaCl solutions (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1421-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, B-71 S.
    Series Statement: U.S. Geological Survey bulletin 1421-B
    Language: English
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  • 79
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    Series available for loan
    The Marquette Range Supergroup in the Gogebic iron district, Michigan and Wisconsin (1980)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1460)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, 96 S.
    Series Statement: U.S. Geological Survey bulletin 1460
    Language: English
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  • 80
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    Series available for loan
    Changes in stratigraphic nomenclature by the U.S. Geological Survey, 1975 (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1222-A)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, A-84 S.
    Series Statement: U.S. Geological Survey bulletin 1422-A
    Language: English
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  • 81
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    Series available for loan
    The Maudlow and Sedan Formations of the Upper Cretaceous Livingston Group on the west edge of the Crazy Mountains basin, Montana (1977)
    Washington, DC : United States Gov. Print. Off.
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    Details Availability
    Call number: SR 90.0001(1422-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, B-68 S.
    Series Statement: U.S. Geological Survey bulletin 1422-B
    Language: English
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  • 82
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    Series available for loan
    Mineral resources of the Bradwell Bay Wilderness and the Sopchoppy River Study Area, Wakulla County, Florida (1977)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1431)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, 37 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1431
    Language: English
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  • 83
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    Series available for loan
    Nomenclature of Precambrian rocks on Colorado (1977)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1422-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, D-22 S.
    Series Statement: U.S. Geological Survey bulletin 1422-D
    Language: English
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  • 84
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    Series available for loan
    Mercury deposits in Turkey (1978)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1456)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, 80 S.
    Series Statement: U.S. Geological Survey bulletin 1456
    Language: English
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  • 85
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    Geology of the Karalar-Yesiller area, northwest Anatolia, Turkey (1980)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1461)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, 72 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1461
    Language: English
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  • 86
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    Monograph available for loan
    The quaternary history of Scandinavia (1995)
    Cambridge : Cambridge Univ. Press
    Details Availability
    Call number: M 97.0238
    Type of Medium: Monograph available for loan
    Pages: 199 S.
    ISBN: 0521417309
    Classification:
    Historical Geology
    Language: English
    Location: Upper compact magazine
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  • 87
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    Monograph available for loan
    Ecology, diversity, taxonomy; Vol. 2. (1996)
    Königstein : Koeltz Scientific Books
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    Call number: M 97.0424 ; AWI Bio-99-0086
    In: Iconographia diatomologica
    Type of Medium: Monograph available for loan
    Pages: 390 S. : zahlr. Ill.
    ISBN: 3874293866
    Classification:
    Paleontology
    Language: English
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    Location: Upper compact magazine
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  • 88
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    Series available for loan
    Shoreline changes along the outer shore of Cape Cod from Long Point to Monomoy Point (1978)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-78/17
    In: CRREL Report, 78-17
    Description / Table of Contents: Abstract: This investigation utilized historical and recent aerial photographs and satellite imagery in 1) estimating changes in positions of the high-water line and sea cliff break and base, in rates of accretion and/or erosion, and in volumes of transported sediment, and 2) providing a preliminary evaluation of the direction of littoral transport along the outer Cape Cod coast. Using aerial photographs acquired in 1938, 1952, 1971 and 1974 with manual photointerpretation techniques, changes in the distances from selected reference points to the cliff break, cliff base and the high-water line were measured. LANDSAT-1 and -2 imagery acquired from 1 September 1972 to 28 May 1975 was evaluated for use in determining the directions of littoral transport that are active the predominant amount of time. Although the imagery has been very useful for this purpose at other locations, it proved to be useless along the outer shore of Cape Cod. Largest net migrations of the high water line from 1938 to 1974 occurred in the northern and southern portions of this coast. The northern maximum high water line was 321.4 ft, the southern was 1794.6 ft. The central portion of the coast was generally more stable with changes varying from 6.8 to 157.6 ft. Cliff-base recession rates varied from 0.4 to 7.3 ft/yr. Maximum estimated net volume of sediment deposited per linear foot of beach from 1938 to 1974 was 334 yd^3 (based on 2 yd^3/ft of recession or accretion); maximum eroded was 914 yd^3. Changes in the configuration of spits were used to evaluate directions of littoral transport since suspended sediment concentrations were generally not sufficient to act as natural tracers of surface currents. Based on the literature and a determination of the portion of the coast perpendicular to the direction of dominant wave approach, the location of the nodal zone for predominant littoral directions of drift probably shifts between the area near Spectacle Pond and North Truro Air Force Station. This investigation has illustrated a photo interpretation technique that is useful in performing a reconnaissance of coastal change. The data obtained from this method can be used to supplement those acquired by ground surveys and are valid as first approximations for planning subsequent, more detailed surveys.
    Type of Medium: Series available for loan
    Pages: vi, 49 Seiten , Illustrationen
    Series Statement: CRREL Report 78-17
    URL: https://hdl.handle.net/11681/9394
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors: U.S. customary to metric units of measurement Introduction Background Previous investigations Analytical procedures Results and discussion Shoreline changes: High-water line Shoreline changes: Cliff recession Volumetric changes Nodal zone location and direction of littoral transport Error evaluation Summary and conclusions Future research Selected bibliography Appendix A: Maps of shoreline with overlays for 1938, 1952, 1971 and 1974 Appendix B: Supplementary data for estimating shoreline change
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  • 89
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    Series available for loan
    The compression of wet snow (1978)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-78/10
    In: CRREL Report, 78-10
    Description / Table of Contents: The compressibility of wet snow is described in terms of pressure melting and nonlinear viscous deformation at grain contacts. The results of experiments with different salinities and liquid water contents are compared with computed densities. The decreasing compressibility of wet snow with increasing salinity and decreasing liquid content is quantified and explained. Simultaneous particle growth and the doubly charged layer at phase boundaries are included in the model. The results show that the density of wet snow increases approximately as a power of time but is highly dependent on the stress, initial particle size, liquid water content, and ionic impurity content of the snow.
    Type of Medium: Series available for loan
    Pages: vi, 23 Seiten , Illustrationen
    Series Statement: CRREL Report 78-10
    URL: https://hdl.handle.net/11681/9405
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Experimental procedure Grain growth Stressed particle contacts Fluid pressure Packing geometry Temperature distribution and heat flow Fluid and impurity flows Results The liquid film Conclusions Literature cited
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  • 90
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    Monograph available for loan
    Sea-level changes : the last 20000 years (1996)
    Chichester [u.a.] : Wiley & Sons
    Details Availability
    Call number: M 97.0285
    Type of Medium: Monograph available for loan
    Pages: xii, 211 Seiten , Illustrationen
    ISBN: 0471969133
    Series Statement: Coastal morphology and research
    Classification:
    Geodynamics
    Language: English
    Note: Contents Preface Acknowledgements Introduction Chapter One: Causes of sea-level change 1.1 Introduction 1.2 Changes in the quantity of oceanic water 1.3 Deformation of the shape of the oceanic basin 1.4 Variations of water density and dynamic changes affecting the water masses Chapter Two: Evidence of former sea levels 2.1 Rocky shores 2.2 Sedimentary shores 2.3 Archaeological and historical sea-level indicators 2.4 Dating a sea-level indicator 2.5 How sea-level curves are constructed Chapter Three: The ice age Earth 3.1 How the last glaciation developed 3.2 The sea-level positions during the last Ice age 3.3 Low-sea-level land bridges and landscapes 3.4 Last glaciation climate and hydrology 3.5 Last glaciation biomass and CO2 exchanges Chapter Four: Deglacial sea-level changes 4.1 Introduction 4.2 Modelling results 4.3 Regional case studies 4.4 A gradually rising or a fluctuating sea level? 4.5 The Younger Dryas sea-level change 4.6 Impacts of past sea-level rise on coastal systems 4.7 Palaeomonsoons Chapter Five: Relative sea-level changes in the late Holocene 5.1 Delta and coral reef development 5.2 Continuance of isostatic emergence / submergence processes 5.3 Seismo-tectonic displacements 5.4 Relative sea-level changes produced by aseismic tectonics 5.5 Transgression-regression sequences and sea-level changes 6 Present-day sea-level trends 6.1 Introduction 6.2 Instrumental measurements . 6.3 Explanation of current estimations of global sea-level rise 6.4 Coastal areas at risk from sea-level rise Conclusions References Author Index Geographical Index Subject Index
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  • 91
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    Monograph available for loan
    Orogeny through time (1997)
    London : The Geological Society
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    Call number: 9/M 97.0291
    In: Geological Society special publication
    Description / Table of Contents: This book presents a series of review articles on nine important ancient orogens on Earth. Comparison of these mountain belts provides a wealth of information for the debate on whether there has been a change in mountain-building processes through the history of the Earth. As a precursor to these papers, the rheology of the Earth’s lithosphere through time is reviewed. Theoretical analysis and insight into the behaviour of the lithosphere of other planets constrain mechanical considerations of the Earth’s lithosphere. It is clear from these overviews that geodynamic concepts and modelling, and new techniques such as deep seismic profiling and geochronology are having a profound impact on orogenic studies. It is also clear that orogenesis must not be equated with the Wilson cycle, culminating in continent-continent collision. Subduction-related orogens and intraplate orogens are also significant.
    Type of Medium: Monograph available for loan
    Pages: 270 S. , Ill., graph. Darst., Kt.
    ISBN: 1897799756
    Series Statement: Geological Society special publication 121
    URL: http://sp.lyellcollection.org/content/121/1
    Classification:
    Tectonics
    Language: English
    Note: Jean-Pierre Burg and Mary Ford: Orogeny through time: an overview / Geological Society, London, Special Publications, 121:1-17, doi:10.1144/GSL.SP.1997.121.01.01 --- Giorgio Ranalli: Rheology of the lithosphere in space and time / Geological Society, London, Special Publications, 121:19-37, doi:10.1144/GSL.SP.1997.121.01.02 --- P. G. Thomas, P. Allemand, and N. Mangold: Rheology of planetary lithospheres: a review from impact cratering mechanics / Geological Society, London, Special Publications, 121:39-62, doi:10.1144/GSL.SP.1997.121.01.03 --- P. Choukroune, J. N. Ludden, D. Chardon, A. J. Calvert, and H. Bouhallier: Archaean crustal growth and tectonic processes: a comparison of the Superior Province, Canada and the Dharwar Craton, India / Geological Society, London, Special Publications, 121:63-98, doi:10.1144/GSL.SP.1997.121.01.04 --- M. G. O’Dea, G. S. Lister, T. Maccready, P. G. Betts, N. H. S. Oliver, K. S. Pound, W. Huang, R. K. Valenta, N. H. S. Oliver, and R. K. Valenta: Geodynamic evolution of the Proterozoic Mount Isa terrain / Geological Society, London, Special Publications, 121:99-122, doi:10.1144/GSL.SP.1997.121.01.05 --- A. G. Milnes, O. P. Wennberg, Ø. Skår, and A. G. Koestler: Contraction, extension and timing in the South Norwegian Caledonides: the Sognefjord transect / Geological Society, London, Special Publications, 121:123-148, doi:10.1144/GSL.SP.1997.121.01.06 --- David R. Gray: Tectonics of the southeastern Australian Lachlan Fold Belt: structural and thermal aspects / Geological Society, London, Special Publications, 121:149-177, doi:10.1144/GSL.SP.1997.121.01.07 --- P. Rey, J.-P. Burg, and M. Casey: The Scandinavian Caledonides and their relationship to the Variscan belt / Geological Society, London, Special Publications, 121:179-200, doi:10.1144/GSL.SP.1997.121.01.08 --- V. N. Puchkov: Structure and geodynamics of the Uralian orogen / Geological Society, London, Special Publications, 121:201-236, doi:10.1144/GSL.SP.1997.121.01.09 --- Simon Lamb, Leonore Hoke, Lorcan Kennan, and John Dewey: Cenozoic evolution of the Central Andes in Bolivia and northern Chile / Geological Society, London, Special Publications, 121:237-264, doi:10.1144/GSL.SP.1997.121.01.10
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  • 92
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    Monograph available for loan
    Rock fractures and fluid flow : contemporary understanding and applications (1996)
    Washington : National Academy Press
    Details Availability
    Call number: M 97.0241
    Type of Medium: Monograph available for loan
    Pages: xvi, 551 S.
    ISBN: 0309049962
    Classification:
    Petrophysics
    Language: English
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  • 93
    Monograph available for loan
    Monograph available for loan
    Developments in petrophysics (1997)
    London : The Geological Society
    Associated volumes
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    Call number: 9/M 97.0287
    In: Geological Society special publication
    Description / Table of Contents: Petrophysics is the study of the physical properties of rocks in the broadest sense. As such it provides the fundamental understanding that enables geologists to describe the physical state of a rock, to predict its behaviour and to interpret geophysical data. Traditionally the emphasis has been on hydrocarbon reservoir evaluation, but it is equally applicable to the evolution of the Earth at all scales. This volume includes developments in pore-scale studies, electrical properties, seismic methods and measurement techniques, as well as reviewing aspects of petrophysical prediction and interpretation.
    Type of Medium: Monograph available for loan
    Pages: VII, 393 S. , Ill., graph. Darst., Kt.
    ISBN: 1897799810
    Series Statement: Geological Society special publication 122
    URL: http://sp.lyellcollection.org/content/122/1
    Classification:
    Petrophysics
    Language: English
    Note: P. D. Jackson, D. G. Gunn, R. C. Flint, D. Beamish, P. I. Meldrum, M. A. Lovell, P. K. Harvey, and A. Peyton: A non-contacting resistivity imaging method for characterizing whole round core while in its liner / Geological Society, London, Special Publications, 122:1-10, doi:10.1144/GSL.SP.1997.122.01.01 --- D. J. Prosser, A. Hurst, and M. R. Wilson: One-man-operable probe permeameters / Geological Society, London, Special Publications, 122:11-18, doi:10.1144/GSL.SP.1997.122.01.02 --- S. R. McDougall, A. B. Dixit, and K. S. Sorbie: Network analogues of wettability at the pore scale / Geological Society, London, Special Publications, 122:19-35, doi:10.1144/GSL.SP.1997.122.01.03 --- S. Pugliese and N. Petford: Pore-structure visualization in microdioritic enclaves / Geological Society, London, Special Publications, 122:37-46, doi:10.1144/GSL.SP.1997.122.01.04 --- Paul B. Basan, Ben D. Lowden, Peter R. Whattler, and John J. Attard: Pore-size data in petrophysics: a perspective on the measurement of pore geometry / Geological Society, London, Special Publications, 122:47-67, doi:10.1144/GSL.SP.1997.122.01.05 --- M. S. King, A. Shakeel, and N. A. Chaudhry: Acoustic wave propagation and permeability in sandstones with systems of aligned cracks / Geological Society, London, Special Publications, 122:69-85, doi:10.1144/GSL.SP.1997.122.01.06 --- Shiyu Xu, Just Doorenbos, Sue Raikes, and Roy White: A simple but powerful model for simulating elastic wave velocities in clastic Silicate rocks / Geological Society, London, Special Publications, 122:87-105, doi:10.1144/GSL.SP.1997.122.01.07 --- T. Apuani, M. S. King, C. Butenuth, and M. H. De Freitas: Measurements of the relationship between Sonic wave velocities and tensile strength in Anisotropic rock / Geological Society, London, Special Publications, 122:107-119, doi:10.1144/GSL.SP.1997.122.01.08 --- C. McCann, J. Sothcott, and S. B. Assefa: Prediction of petrophysical properties from seismic quality factor measurements / Geological Society, London, Special Publications, 122:121-130, doi:10.1144/GSL.SP.1997.122.01.09 --- Y. F. Sun and D. Goldberg: Estimation of aspect-ratio changes with pressure from seismic velocities / Geological Society, London, Special Publications, 122:131-139, doi:10.1144/GSL.SP.1997.122.01.10 --- P. K. Harvey, M. A. Lovell, J. C. Lofts, P. A. Pezard, and J. F. Bristow: Petrophysical estimation from downhole Mineralogy logs / Geological Society, London, Special Publications, 122:141-157, doi:10.1144/GSL.SP.1997.122.01.11 --- Paul F. Worthington: Petrophysical estimation of permeability as a function of scale / Geological Society, London, Special Publications, 122:159-168, doi:10.1144/GSL.SP.1997.122.01.12 --- C. A. Gonçalves, P. K. Harvey, and M. A. Lovell: Prediction of petrophysical parameter logs using a multilayer backpropagation neural network / Geological Society, London, Special Publications, 122:169-180, doi:10.1144/GSL.SP.1997.122.01.13 --- Brian P. Moss: The partitioning of petrophysical data: a review / Geological Society, London, Special Publications, 122:181-252, doi:10.1144/GSL.SP.1997.122.01.14 --- A. Revil, P. A. Pezard, and M. Darot: Electrical conductivity, spontaneous potential and ionic diffusion in porous media / Geological Society, London, Special Publications, 122:253-275, doi:10.1144/GSL.SP.1997.122.01.15 --- Brígida Ramati P. Da Rocha and Tarek M. Habashy: Fractal Geometry, porosity and complex resistivity: from rough pore interfaces to hand specimens / Geological Society, London, Special Publications, 122:277-286, doi:10.1144/GSL.SP.1997.122.01.16 --- Brígida Ramati P. Da Rocha and Tarek M. Habashy: Fractal Geometry, porosity and complex resistivity: from hand specimen to field data / Geological Society, London, Special Publications, 122:287-297, doi:10.1144/GSL.SP.1997.122.01.17 --- M. Ben Clennell: Tortuosity: a guide through the maze / Geological Society, London, Special Publications, 122:299-344, doi:10.1144/GSL.SP.1997.122.01.18 --- J. C. Lofts, J. Bedford, H. Boulton, J. A. van Doorn, and P. Jeffreys: Feature recognition and the interpretation of images acquired from horizontal wellbores / Geological Society, London, Special Publications, 122:345-365, doi:10.1144/GSL.SP.1997.122.01.19 --- D. Goldberg and Y. F. Sun: Scattering attenuation as a function of depth in the Upper Oceanic Crust / Geological Society, London, Special Publications, 122:367-375, doi:10.1144/GSL.SP.1997.122.01.20 --- N. Passas, C. Butenuth, and M. H. De Freitas: An application of the Moiré Method to a study of local strains during rock failure in tension / Geological Society, London, Special Publications, 122:377-388, doi:10.1144/GSL.SP.1997.122.01.21
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  • 94
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    Monograph available for loan
    Tectonic evolution of Southeast Asia (1996)
    London : The Geological Society
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    Call number: 9/M 97.0293
    In: Geological Society special publication
    Description / Table of Contents: SE Asia is probably the finest natural geological laboratory in the world, yet is still not geologically well known. It is a spectacular region in which the manifestations and processes of plate collision can be observed at present and in which their history is recorded. It is a region that must be understood if we are to understand mountain belts, arc development marginal basin evolution and, more generally, the behaviour of the lithosphere in collision settings. Furthermore, the region is developing rapidly on the economic front, and a major part of this rapid development is built on natural resources. The geological reasons for the distribution of these resources are therefore of major importance for the inhabitants of the region and for any attempts to discover and exploit them. The volume will be of interest to all geologists working in SE Asia, particularly those involved in the petroleum industry.
    Type of Medium: Monograph available for loan
    Pages: XIII, 566 S. , Ill., graph. Darst., Kt.
    ISBN: 1897799527
    Series Statement: Geological Society special publication 106
    URL: http://sp.lyellcollection.org/content/106/1
    Classification:
    Regional Geology
    Language: English
    Note: Robert Hall, D. J. Blundell, and Robert Hall: Tectonic evolution of SE Asia: introduction / Geological Society, London, Special Publications, 106:vii-xiii, doi:10.1144/GSL.SP.1996.106.01.01 --- Part 1: Present-day Tectonics --- Robert McCaffrey: Slip partitioning at convergent plate boundaries of SE Asia / Geological Society, London, Special Publications, 106:3-18, doi:10.1144/GSL.SP.1996.106.01.02 --- Jacques André Malod and Badrul Mustafa Kemal: The Sumatra margin: oblique subduction and lateral displacement of the accretionary prism / Geological Society, London, Special Publications, 106:19-28, doi:10.1144/GSL.SP.1996.106.01.03 --- Claude Rangin, Daharta Dahrin, Ray Quebral, and The Modec Scientific Party: Collision and strike-slip faulting in the northern Molucca Sea (Philippines and Indonesia): preliminary results of a morphotectonic study / Geological Society, London, Special Publications, 106:29-46, doi:10.1144/GSL.SP.1996.106.01.04 --- A. N. Richardson, D. J. Blundell, and A. N. Richardson: Continental collision in the Banda arc / Geological Society, London, Special Publications, 106:47-60, doi:10.1144/GSL.SP.1996.106.01.05 --- David B. Snyder, John Milsom, and Hardi Prasetyo: Geophysical evidence for local indentor tectonics in the Banda arc east of Timor / Geological Society, London, Special Publications, 106:61-73, doi:10.1144/GSL.SP.1996.106.01.06 --- B. D. Hughes, K. Baxter, R. A. Clark, and D. B. Snyder: Detailed processing of seismic reflection data from the frontal part of the Timor trough accretionary wedge, eastern Indonesia / Geological Society, London, Special Publications, 106:75-83, doi:10.1144/GSL.SP.1996.106.01.07 --- John Milsom, Steve Kaye, and Sardjono: Extension, collision and curvature in the eastern Banda arc / Geological Society, London, Special Publications, 106:85-94, doi:10.1144/GSL.SP.1996.106.01.08 --- Part 2: Tectonic Development of Southeast Asia --- I. Metcalfe: Pre-Cretaceous evolution of SE Asian terranes / Geological Society, London, Special Publications, 106:97-122, doi:10.1144/GSL.SP.1996.106.01.09 --- Gordon Packham: Cenozoic SE Asia: reconstructing its aggregation and reorganization / Geological Society, London, Special Publications, 106:123-152, doi:10.1144/GSL.SP.1996.106.01.10 --- Robert Hall: Reconstructing Cenozoic SE Asia / Geological Society, London, Special Publications, 106:153-184, doi:10.1144/GSL.SP.1996.106.01.11 --- T. O. Simandjuntak and A. J. Barber: Contrasting tectonic styles in the Neogene orogenic belts of Indonesia / Geological Society, London, Special Publications, 106:185-201, doi:10.1144/GSL.SP.1996.106.01.12 --- Bryan Richter and Michael Fuller: Palaeomagnetism of the Sibumasu and Indochina blocks: implications for the extrusion tectonic model / Geological Society, London, Special Publications, 106:203-224, doi:10.1144/GSL.SP.1996.106.01.13 --- Robert B. Stokes, Paul F. Lovatt Smith, and Ko Soumphonphakdy: Timing of the Shan-Thai-Indochina collision: new evidence from the Pak Lay Foldbelt of the Lao PDR / Geological Society, London, Special Publications, 106:225-232, doi:10.1144/GSL.SP.1996.106.01.14 --- Paul F. Lovatt Smith, Robert B. Stokes, Charlie Bristow, and Andrew Carter: Mid-Cretaceous inversion in the Northern Khorat Plateau of Lao PDR and Thailand / Geological Society, London, Special Publications, 106:233-247, doi:10.1144/GSL.SP.1996.106.01.15 --- Charles S. Hutchison: The ‘Rajang accretionary prism’ and ‘Lupar Line’ problem of Borneo / Geological Society, London, Special Publications, 106:247-261, doi:10.1144/GSL.SP.1996.106.01.16 --- Shariff A. K. Omang and A. J. Barber: Origin and tectonic significance of the metamorphic rocks associated with the Darvel Bay Ophiolite, Sabah, Malaysia / Geological Society, London, Special Publications, 106:263-279, doi:10.1144/GSL.SP.1996.106.01.17 --- Khalid Ngah, Mazlan Madon, and H. D. Tjia: Role of pre-Tertiary fractures in formation and development of the Malay and Penyu basins / Geological Society, London, Special Publications, 106:281-289, doi:10.1144/GSL.SP.1996.106.01.18 --- H. D. Tjia and K. K. Liew: Changes in tectonic stress field in northern Sunda Shelf basins / Geological Society, London, Special Publications, 106:291-306, doi:10.1144/GSL.SP.1996.106.01.19 --- Ben Clennell: Far-field and gravity tectonics in Miocene basins of Sabah, Malaysia / Geological Society, London, Special Publications, 106:307-320, doi:10.1144/GSL.SP.1996.106.01.20 --- W. J. McCourt, M. J. Crow, E. J. Cobbing, and T. C. Amin: Mesozoic and Cenozoic plutonic evolution of SE Asia: evidence from Sumatra, Indonesia / Geological Society, London, Special Publications, 106:321-335, doi:10.1144/GSL.SP.1996.106.01.21 --- M. A. Samuel and N. A. Harbury: The Mentawai fault zone and deformation of the Sumatran Forearc in the Nias area / Geological Society, London, Special Publications, 106:337-351, doi:10.1144/GSL.SP.1996.106.01.22 --- Koji Wakita, Jan Sopaheluwakan, Kazuhiro Miyazaki, Iskandar Zulkarnain, and Munasri: Tectonic evolution of the Bantimala Complex, South Sulawesi, Indonesia / Geological Society, London, Special Publications, 106:353-364, doi:10.1144/GSL.SP.1996.106.01.23 --- Moyra E. J. Wilson and Dan W. J. Bosence: The Tertiary evolution of South Sulawesi: a record in redeposited carbonates of the Tonasa Limestone Formation / Geological Society, London, Special Publications, 106:365-389, doi:10.1144/GSL.SP.1996.106.01.24 --- Steven C. Bergman, Dana Q. Coffield, James P. Talbot, and Richard A. Garrard: Tertiary Tectonic and magmatic evolution of western Sulawesi and the Makassar Strait, Indonesia: evidence for a Miocene continent-continent collision / Geological Society, London, Special Publications, 106:391-429, doi:10.1144/GSL.SP.1996.106.01.25 --- Jason R. Ali, John Milsom, Edward M. Finch, and Bundan Mubroto: SE Sundaland accretion: palaeomagnetic evidence of large Plio-Pleistocene thin-skin rotations in Buton / Geological Society, London, Special Publications, 106:431-443, doi:10.1144/GSL.SP.1996.106.01.26 --- P Z. Vroon, M. J. Van Bergen, and E. J. Forde: Pb and Nd isotope constraints on the provenance of tectonically dispersed continental fragments in east Indonesia / Geological Society, London, Special Publications, 106:445-453, doi:10.1144/GSL.SP.1996.106.01.27 --- Kees Linthout, Henk Helmers, Jan R. Wijbrans, and Jan Diederik A. M. Van Wees: 40Ar/39Ar constraints on obduction of the Seram ultramafic complex: consequences for the evolution of the southern Banda Sea / Geological Society, London, Special Publications, 106:455-464, doi:10.1144/GSL.SP.1996.106.01.28 --- Tim R. Charlton: Correlation of the Salawati and Tomori Basins, eastern Indonesia: a constraint on left-lateral displacements of the Sorong fault zone / Geological Society, London, Special Publications, 106:465-481, doi:10.1144/GSL.SP.1996.106.01.29 --- Jeffrey F. A. Malaihollo and Robert Hall: The geology and tectonic evolution of the Bacan region, east Indonesia / Geological Society, London, Special Publications, 106:483-497, doi:10.1144/GSL.SP.1996.106.01.30 --- Simon Baker and Jeffrey Malaihollo: Dating of Neogene igneous rocks in the Halmahera region: arc initiation and development / Geological Society, London, Special Publications, 106:499-509, doi:10.1144/GSL.SP.1996.106.01.31 --- M. Pubellier, R. Quebral, M. Aurelio, and C. Rangin: Docking and post-docking escape tectonics in the southern Philippines / Geological Society, London, Special Publications, 106:511-523, doi:10.1144/GSL.SP.1996.106.01.32 --- P. V. Crowhurst, K. C. Hill, D. A. Foster, and A. P. Bennett: Thermochronological and geochemical constraints on the tectonic evolution of northern Papua New Guinea / Geological Society, London, Special Publications, 106:525-537, doi:10.1144/GSL.SP.1996.106.01.33 --- Helmut Wopfner: Gondwana origin of the Baoshan and Tengchong terranes of west Yunnan / Geological Society, London, Special Publications, 106:539-547, doi:10.1144/GSL.SP.19
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  • 95
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    Series available for loan
    The prediction of unfrozen water contents in frozen soils from liquid limit determinations (1976)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-76/8
    In: CRREL Report, 76-8
    Description / Table of Contents: During the past decade a number of methods for measuring the amount of unfrozen water in partially frozen ground have emerged. Means of quickly and simply predicting unfrozen water contents in clay have become increasingly important with the growth of interest in encapsulating clay soils compacted at low water contents to serve as base courses for roads. Unfortunately the measurements require sophisticated equipment and, in most instances, specially trained operators. In an effort to simplify the task of obtaining water-ice phase composition data, methods of calculating phase composition curves from other, simpler measurements on soils have been sought. The paper presents a method of deriving the measurement of unfrozen water contents at various temperatures from liquid limit determinations.
    Type of Medium: Series available for loan
    Pages: iv, 9 Seiten , Illustrationen
    Series Statement: CRREL Report 76-8
    URL: https://apps.dtic.mil/docs/citations/ADA026632
    Language: English
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  • 96
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    Series available for loan
    Site access for a subarctic research effort (1976)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-76/9
    In: CRREL Report, 76-9
    Description / Table of Contents: Access to study areas may be an important factor in long-term field-oriented research, particularly in-regions without well-developed road and communications systems. In a wildland hydrometeorology research project in subarctic Alaska, access to and within a 40-square-mile research watershed has been developed both in accordance with a general plan prepared at project inception and in response to developing research requirements. Foot trails, trails for 'off-road' low-ground-pressure tracked vehicles, helicopter transport, long-term data recorders, and radio telemetry of data have all been incorporated in an access and communications system. Cost estimates indicate that incorporation of gravel roads into the system would be economically advantageous, given adequate funding for initial road construction.
    Type of Medium: Series available for loan
    Pages: iv, 9 Seiten , Illustrationen
    Series Statement: CRREL Report 76-9
    URL: https://apps.dtic.mil/docs/citations/ADA026624
    Language: English
    Note: Contents Abstract Preface Conversion factors for U.S. customary and SI units Introduction Access within the Caribou-Poker Creeks Research Watershed Trail access Helicopter access Road access Alternative approaches Long-term recorders Telemetry systems Remote sensing Relative costs A desirable system Selected bibliography
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  • 97
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    Cantilever beam tests on reinforced ice (1976)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-76/7
    In: CRREL Report, 76-7
    Description / Table of Contents: This report covers a series of cantilever beam tests designed to determined the efficacy of adding reinforcement to an ice cover. Tests were run using 1-in.-diam tree branches, 3/16-in.-diam wire rope and 9/16-in. half-round wood dowels as reinforcement for both seawater and freshwater ice. The results show a definite advantage derived from using reinforcement, even when poorly placed. The results also show that reinforced ice carries a load even after it cracks. Thus, after the initial cracks there is time to remove people and equipment before final breakthrough. One must bear in mind, however, that reinforcement has disadvantages. The darker reinforcement absorbs solar radiation and thereby causes earlier weakening of the ice cover. Also, in many cases the time and effort required to place reinforcement may exceed those required to achieve equal strength by additional thickening of the ice sheet. This study has shown that understanding of the failure mechanism of ice under repetitive loading is poor and that future studies should be performed on this problem. Also, this study covered only cantilever beams. The actual field problem is strengthening a three-dimensional sheet. Hence, distribution and orientation of the reinforcement should be addressed in future studies.
    Type of Medium: Series available for loan
    Pages: v, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 76-7
    URL: https://cdm16021.contentdm.oclc.org/digital/collection/p266001coll1/id/6219
    Language: English
    Note: Contents Abstract Preface Summary Conversion factors: U.S. customary to SI metric units Introduction Typical methods of constructing ice bridges Current knowledge Test program Objectives Equipment Procedure Data General Specific ice sheets Test results Conclusions Recommendations Literature cited
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    Branch Library: AWI Library
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  • 98
    Series available for loan
    Series available for loan
    De-icing using lasers (1976)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-201-76/10
    In: CRREL Report, 76-10
    Type of Medium: Series available for loan
    Pages: vi, 25 Seiten , Illustrationen
    Series Statement: CRREL Report 76-10
    URL: https://cdm16021.contentdm.oclc.org/digital/collection/p266001coll1/id/6144
    Language: English
    Note: CONTENTS Introduction Experimental work SCR samples CAG samples CMS samples UAG samples SI samples Optical system Equipment Procedure Photographic work Large cracks and fissures Small damage to the surface Small damage to the buIk Results Damage as a function of the position x of the focal point; n(x) Damage as a function of the number of irradiations #; n(#) Damage as a function of crystallographic orientation ĉ; n (ĉ); p (ĉ) Damage as a function of surface structure Damage as a function of age A; n (A) Damage as a function of wavelength λ; p(λ) Systematic study of damage as a function of W, t, m and s; n(W, t, m, s) Analysis Fracture in ice Mechanisms for optically generated damage in transparent dielectrics Discussion of the results Summary and conclusions Literature cited
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  • 99
    Monograph available for loan
    Monograph available for loan
    Resources and environment world atlas; Vol. 2 (1998)
    Vienna : Ed. Hölzel
    Associated volumes
    Details Availability
    Call number: PIK L 010-99-0029/2 ; MOP A3 17-6054-2
    In: Resources and environment world atlas, Vol. 2
    Type of Medium: Monograph available for loan
    Pages: 190 Bl., Bl. a - l , überw. Kt.
    Edition: 1. ed.
    Language: English , Russian
    Note: Teilw. in kyrill. Schr.
    Location: A 18 - must be ordered
    Location: MOP - must be ordered
    Branch Library: PIK Library
    Branch Library: GFZ Library
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  • 100
    Monograph available for loan
    Monograph available for loan
    Encyclopedia of planetary sciences (1997)
    London [u.a.] : Chapman & Hall
    Details Availability
    Call number: 4/M 97.0295
    Type of Medium: Monograph available for loan
    Pages: 990 S. + CD-ROM
    ISBN: 0412069512
    Series Statement: Encyclopedia of earth sciences series
    Classification:
    Astronomy and Astrophysics
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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