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  • Washington, DC : United States Gov. Print. Off.
  • 2005-2009  (32)
  • 1970-1974  (517)
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Year
  • 1
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: S 90.0002(1766)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: XVI, 225 S. : Ill
    ISBN: 9781411325159
    Series Statement: U.S. Geological Survey professional paper 1766 : Groundwater Resources Program
    Classification:
    Hydrology
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: S 90.0002(1386-K) ; AWI G7-11-0051
    In: Satellite image atlas of glaciers of the world
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: XXVI, K 525 S. , zahlr. Ill., graph. Darst., Kt.
    ISBN: 9780607982916
    Series Statement: Satellite image atlas of glaciers of the world / ed. by Richard S. Williams ... K
    Classification:
    Regional Geology
    Note: Erscheinungsjahr in Vorlageform:2008
    Location: Lower compact magazine
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Branch Library: AWI Library
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  • 3
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: S 90.0002(1762)
    In: Professional paper
    Description / Table of Contents: Augustine Island (volcano) in lower Cook Inlet, Alaska, has erupted repeatedly in late-Holocene and historical times. Eruptions typically beget high-energy volcanic processes. Most notable are bouldery debris avalanches containing immense angular clasts shed from summit domes. Coarse deposits of these avalanches form much of Augustines lower flanks. A new geologic map at 1:25,000 scale depicts these deposits, these processes. We correlate deposits by tephra layers calibrated by many radiocarbon dates.Augustine Volcano began erupting on the flank of a small island of Jurassic clastic-sedimentary rock before the late Wisconsin glaciation (late Pleistocene). The oldest known effusions ranged from olivine basalt explosively propelled by steam, to highly explosive magmatic eruptions of dacite or rhyodacite shed as pumice flows. Late Wisconsin piedmont glaciers issuing from the mountainous western mainland surrounded the island while dacitic eruptive debris swept down the south volcano flank.
    Type of Medium: Series available for loan
    Pages: VII, 78 S. + 2 Kt.-Beil. , Ill., graph. Darst., Kt. , 2 Kt.-Beil. , 28 cm
    ISBN: 9781411324114 , 1-411-32411-0
    Series Statement: U.S. Geological Survey professional paper 1762
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 4
    Call number: S 90.0002(1761)
    In: Professional paper
    Description / Table of Contents: The southern Española basin consists of a westward- and northward-thickening wedge of rift fill, composed primarily of Santa Fe Group sediments, that serves as an important aquifer for the city of Santa Fe and surrounding areas. Detailed aeromagnetic surveys were flown to better understand ground-water resources in this aquifer. This report presents a synthesis of these data with gravity data and other constraints. The interpretations were accomplished using qualitative interpretation, state-of-art data analysis techniques, and two- and three-dimensional modeling. The results depict the presence of and depth to many geologic features that have hydrogeologic significance, including shallow faults, different types of igneous units, and basement rocks. The results are presented as map interpretations, geophysical profile models, and a digital surface that represents the base and thickness of Santa Fe Group sediments, as well as vector files of some volcanic features and faults.
    Type of Medium: Series available for loan
    Pages: VI, 87 S. : Ill., graph. Darst. + 1 Kt.-Beil. , 1 CD-ROM
    ISBN: 9781411323650 , 1-411-32365-3
    Series Statement: U.S. Geological Survey professional paper 1761
    Classification:
    Regional Geology
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 5
    Call number: S 90.0002(1703)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: VII, 414 S. : farb. Ill., farb. Kt.
    ISBN: 9781411321656
    Series Statement: U.S. Geological Survey professional paper 1703
    Classification:
    Hydrology
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 6
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: S 90.0002(1650-E)
    In: Atlas of relations between climatic parameters and distributions of import trees and shrubs in North America
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: CD-ROM
    Edition: Vers. 1.0
    Series Statement: 1650-E
    Classification:
    Historical Geology
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 7
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: S 90.0002(1764)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: V, 21 S. , Ill., graph. Darst. , 28 cm
    Series Statement: U.S. Geological Survey professional paper 1764
    Classification:
    Regional Geology
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 8
    Call number: S 90.0002(1758)
    In: Professional paper
    Description / Table of Contents: Comparing altered wetlands to natural wetlands in the same region improves the ability to interpret the gradual and cumulative effects of human development on freshwater wetlands. Hydrologic differences require explicit attention because they affect nearly all wetland functions and are an overriding influence on other comparisons involving wetland water quality and ecology. This study adopts several new approaches to quantify wetland hydrologic characteristics and then describes and compares the hydrology, water quality, and ecology of 10 isolated freshwater marsh and cypress wetlands in the mantled karst landscape of central Florida. Four of the wetlands are natural, and the other six have water levels indirectly lowered by ground-water withdrawals on municipally owned well fields. For several decades, the water levels in four of these altered wetlands have been raised by adding ground water in a mitigation process called augmentation. The two wetlands left unaugmented were impaired because their water levels were lowered. Multifaceted comparisons between the altered and natural wetlands are used to examine differences between marshes and cypress wetlands and to describe the effects of augmentation practices on the wetland ecosystems.
    Type of Medium: Series available for loan
    Pages: x, 152 S. , col. ill., col. maps ; 28 cm
    ISBN: 9781411323537
    Series Statement: U.S. Geological Survey professional paper 1758
    Classification:
    Ecology
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 9
    Call number: S 90.0002(1767)
    In: Professional paper
    Description / Table of Contents: Hydrogeologic setting -- Mine flooding and aftermath -- Flooding and formation of rubble chimneys -- Water-level recovery and migration of brine -- Interception of brine and saline water -- Geochemical modeling -- Inverse models -- Forward models -- Discussion of results from geochemical modeling -- Simulated migration of brine and saline water during recovery of water levels -- One-dimensional flow -- Three-dimensional flow -- Model design -- Model calibration -- Model results -- Discussion of results -- Simulated pumping of brine and saline water -- Model design -- Model results -- Model sensitivity -- Discussion of results -- Implications for future mitigation efforts -- Current conditions in the collapse area -- Considerations for future mitigation
    Type of Medium: Series available for loan
    Pages: VII, 51 S. , graph. Darst., Kt.
    ISBN: 9781411325029
    Series Statement: U.S. Geological Survey professional paper 1767
    Note: Erscheinungsjahr in Vorlageform:2009
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 10
    Call number: S 90.0002(1730
    In: Professional paper
    Description / Table of Contents: The Gogebic iron range is an elongate belt of Paleoproterozoic strata extending from the west shore of Lake Gogebic in the upper peninsula of Michigan for about 125 km westward into northern Wisconsin. It is one of six major informally named iron ranges in the Lake Superior region and produced about 325 million tons of direct-shipping ore between 1887 and 1967. A significant resource of concentrating-grade ore remains in the western and eastern parts of the range.The iron range forms a broad, gently southward-opening arc where the central part of the range exposes rocks that were deposited somewhat north of the eastern and western parts. A fundamental boundary marking both the tectonic setting of deposition and the later deformation within the Penokean orogen lies fortuitously in an east-west direction along the range so that the central part of the range preserves sediments deposited north of that boundary, whereas the eastern and western parts of the range were deposited south of the boundary. Thus, the central part of the range provides a record of sedimentation and very mild deformation in a part of the Penokean orogen farthest from the interior of the orogen to the south. The eastern and western parts of the range, in contrast, exhibit a depositional and deformational style typical of parts closer to the interior of the orogen. A second fortuitous feature of the iron range is that the entire area was tilted from 40° to 90° northward by Mesoproterozoic deformation so that the map view offers an oblique cross section of the Paleoproterozoic sedimentary sequence and structures. Together, these features make the Gogebic iron range a unique area in which to observe (1) the lateral transition from deposition on a stable platform to deposition in a tectonically and volcanically active region, and (2) the transition from essentially undeformed Paleoproterozoic strata to their folded and faulted equivalents.
    Type of Medium: Series available for loan
    Pages: V, 44 S. + 1 Kt.-Beil. , Ill., graph. Darst., Kt. , 28 cm
    ISBN: 9781411319172
    Series Statement: U.S. Geological Survey professional paper 1730
    Location: Lower compact magazine
    Branch Library: GFZ Library
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