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  • 1
    Call number: M 93.0049 ; M 547
    Type of Medium: Monograph available for loan
    Pages: X, 285 S. : graph. Darst.
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge Univ. Press
    Call number: M 92.0342 ; M 92.0449
    Type of Medium: Monograph available for loan
    Pages: XXIV, 408 S. : Ill.
    Edition: 1. publ.
    ISBN: 0521380839
    Classification:
    Petrology, Petrography
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 3
    Call number: G 5897 ; 9826
    Type of Medium: Monograph available for loan
    Pages: XVI, 405 S. : Ill., graph. Darst.
    ISBN: 0444414622
    Location: Upper compact magazine
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 4
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    ANU Press
    Publication Date: 2024-03-23
    Description: "Mount Lamington broke out in violent eruption on 21 January 1951, killing thousands of Orokaiva people, devastating villages and destroying infrastructure. Generations of Orokaiva people had lived on the rich volcanic soils of Mount Lamington, apparently unaware of the deadly volcanic threat that lay dormant beneath them. Also unaware were the Europeans who administered the Territory of Papua and New Guinea at the time of the eruption, and who were uncertain about how to interpret the increasing volcanic unrest on the mountain in the preceding days of the disaster. Roars from the Mountain seeks to address why so many people died at Mount Lamington by examining the large amount of published and unpublished records that are available on the 1951 disaster. The information sources also include the results of interviews with survivors and with people who were part of the relief, recovery and remembrance phases of what can still be regarded as one of Australia’s greatest natural-hazard disasters."
    Keywords: Mount Lamington ; volcano ; colonial history ; Papua New Guinea ; Australia ; thema EDItEUR::1 Place qualifiers::1M Australasia, Oceania, Pacific Islands, Atlantic Islands::1MK Oceania::1MKL Melanesia::1MKLP New Guinea::1MKLPN Papua New Guinea ; thema EDItEUR::W Lifestyle, Hobbies and Leisure::WN Nature and the natural world: general interest::WNW The Earth: natural history: general interest ; thema EDItEUR::N History and Archaeology::NH History::NHM Australasian and Pacific history
    Language: English
    Format: image/jpeg
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  • 5
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    ANU Press | ANU Press
    Publication Date: 2024-04-02
    Description: Wally Johnson and Neville Threlfall re-examine the explosive volcanic eruptions that in 1937–43 killed more than 500 people in the Rabaul area of East New Britain, Papua New Guinea. They reassess this disaster in light of the prodigious amount of new scientific and disaster-management work that has been undertaken there since about 1971, when strong tectonic earthquakes shook the area. Comparisons are made in particular with volcanic eruptions in 1994–2014, when half of Rabaul town was destroyed and then abandoned. A striking feature of historical eruptive periods at Rabaul is the near‑simultaneous activity at Vulcan and Tavurvur volcanoes, on either side of Rabaul Harbour. Such rare 'twin' eruptions are interpreted to be the result of a common magma reservoir beneath the harbour. This interpretation has implications for ongoing hazard and risk assessments and for volcano monitoring in the area.
    Keywords: Rabaul ; Volcanic eruptions ; Disaster risk reduction ; New Britain ; Volcanological Observatory ; thema EDItEUR::N History and Archaeology::NH History::NHM Australasian and Pacific history ; thema EDItEUR::J Society and Social Sciences::JB Society and culture: general ; thema EDItEUR::R Earth Sciences, Geography, Environment, Planning::RB Earth sciences::RBC Volcanology and seismology
    Language: English
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  • 6
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    ANU Press
    Publication Date: 2024-04-14
    Description: Volcanic eruptions have killed thousands of people and damaged homes, villages, infrastructure, subsistence gardens, and hunting and fishing grounds in Papua New Guinea and the Solomon Islands. The central business district of a town was destroyed by a volcanic eruption in the case of Rabaul in 1994. Volcanic disasters litter not only the recent written history of both countries—particularly Papua New Guinea—but are recorded in traditional stories as well. Furthermore, evidence for disastrous volcanic eruptions many times greater than any witnessed in historical times is to be found in the geological record. Volcanic risk is greater today than at any time previously because of larger, mainly sedentary populations on or near volcanoes in both countries. An attempt is made in this book to review what is known about past volcanic eruptions and disasters with a view to determining how best volcanic risk can be reduced today in this tectonically complex and volcanically threatening region
    Keywords: emergency management ; papua new guinea ; solomon islands ; volcanic eruptions ; Caldera ; Earthquake ; Rabaul ; thema EDItEUR::W Lifestyle, Hobbies and Leisure::WN Nature and the natural world: general interest::WNW The Earth: natural history: general interest
    Language: English
    Format: image/jpeg
    Format: image/jpeg
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  • 7
    Publication Date: 1952-08-15
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 8
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2011. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry Geophysics Geosystems 12 (2011): Q11003, doi:10.1029/2011GC003689.
    Description: The Galapagos triple junction is not a simple ridge-ridge-ridge (RRR) triple junction. The Cocos-Nazca Rift (C-N Rift) tip does not meet the East Pacific Rise (EPR). Instead, two secondary rifts form the link: Incipient Rift at 2°40′N and Dietz Deep volcanic ridge, the southern boundary of the Galapagos microplate (GMP), at 1°10′N. Recently collected bathymetry data are used to investigate the regional tectonics prior to the establishment of the GMP (∼1.5 Ma). South of C-N Rift a band of northeast-trending cracks cuts EPR-generated abyssal hills. It is a mirror image of a band of cracks previously identified north of C-N Rift on the same age crust. In both areas, the western ends of the cracks terminate against intact abyssal hills suggesting that each crack initiated at the EPR spreading center and cut eastward into pre-existing topography. Each crack formed a short-lived triple junction until it was abandoned and a new crack and triple junction initiated nearby. Between 2.5 and 1.5 Ma, the pattern of cracking is remarkably symmetric about C-N Rift providing support for a crack interaction model in which crack initiation at the EPR axis is controlled by stresses associated with the tip of the westward-propagating C-N Rift. The model also shows that offsets of the EPR axis may explain times when cracking is not symmetric. South of C-N Rift, cracks are observed on seafloor as old as 10.5 Ma suggesting that this triple junction has not been a simple RRR triple junction during that time.
    Description: HS was supported by the U.S. National Science Foundation (NSF) grant OCE‐0751831, DS by NSF grant OCE‐1028537, WZ by NSF grant EAR‐1056317, and LM by NSF grant EAR‐0911151.
    Description: 2012-05-08
    Keywords: East Pacific Rise ; Galapagos triple junction ; Crack propagation ; Triple junction
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 9
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2014. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry, Geophysics, Geosystems 15 (2014): 4692–4711, doi:10.1002/2014GC005563.
    Description: A multifaceted study of the slow spreading Mid-Atlantic Ridge (MAR) at 16.5°N provides new insights into detachment faulting and its evolution through time. The survey included regional multibeam bathymetry mapping, high-resolution mapping using AUV Sentry, seafloor imaging using the TowCam system, and an extensive rock-dredging program. At different times, detachment faulting was active along ∼50 km of the western flank of the study area, and may have dominated spreading on that flank for the last 5 Ma. Detachment morphologies vary and include a classic corrugated massif, noncorrugated massifs, and back-tilted ridges marking detachment breakaways. High-resolution Sentry data reveal a new detachment morphology; a low-angle, irregular surface in the regional bathymetry is shown to be a finely corrugated detachment surface (corrugation wavelength of only tens of meters and relief of just a few meters). Multiscale corrugations are observed 2–3 km from the detachment breakaway suggesting that they formed in the brittle layer, perhaps by anastomosing faults. The thin wedge of hanging wall lavas that covers a low-angle (6°) detachment footwall near its termination are intensely faulted and fissured; this deformation may be enhanced by the low angle of the emerging footwall. Active detachment faulting currently is limited to the western side of the rift valley. Nonetheless, detachment fault morphologies also are present over a large portion of the eastern flank on crust 〉2 Ma, indicating that within the last 5 Ma parts of the ridge axis have experienced periods of two-sided detachment faulting.
    Description: This work was supported by the National Science Foundation grant OCE-1155650.
    Description: 2015-06-05
    Keywords: Oceanic detachment faults ; AUV Sentry ; Mid-Atlantic Ridge
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 10
    Publication Date: 2022-05-25
    Description: Author Posting. © Nature Publishing Group, 2006. This is the author's version of the work. It is posted here by permission of Nature Publishing Group for personal use, not for redistribution. The definitive version was published in Nature 442 (2006): 440-443, doi:10.1038/nature04950.
    Description: Oceanic core complexes are massifs in which lower crustal and upper mantle rocks are exposed at the sea floor. They form at mid-ocean ridges through slip on detachment faults rooted below the spreading axis. To date, most studies of core complexes have been based on isolated inactive massifs that have spread away from ridge axes. A new survey of the Mid-Atlantic Ridge (MAR) near 13°N reveals a segment in which a number of linked detachment faults extend for 75 km along one flank of the spreading axis. The detachment faults are apparently all currently active and at various stages of development. A field of extinct core complexes extends away from the axis for at least 100 km. The new data document the topographic characteristics of actively-forming core complexes and their evolution from initiation within the axial valley floor to maturity and eventual inactivity. Within the surrounding region there is a strong correlation between detachment fault morphology at the ridge axis and high rates of hydroacoustically-recorded earthquake seismicity. Preliminary examination of seismicity and seafloor morphology farther north along the MAR suggests that active detachment faulting is occurring in many segments and that detachment faulting is more important in the generation of ocean crust at this slow-spreading ridge than previously suspected.
    Description: This work was supported by the National Science Foundation.
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: 3005310 bytes
    Format: application/pdf
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