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  • 1
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    The Royal Forest & Bird Protection Society of New Zealand
    In:  The Royal Forest & Bird Protection Society of New Zealand, Wellington, New Zealand, 72 pp. ISBN 978-0-473-28521-0
    Publication Date: 2019-06-28
    Type: Book , NonPeerReviewed
    Format: text
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  • 2
    Publication Date: 2023-01-19
    Description: About 10% of Europe's surface area is prone to rapid flooding of rivers confined in valleys. The devastating potential of such floods is exacerbated by the deficits of existing gauging networks, including low station densities and recording frequencies, and lack of information beyond stage height. Here, we use seismic data of the July 2021 Ahrtal flood, Germany, to extract information to complement sparse hydrometric data, and to reconstruct the rapid evolution of this fatal event. We show that a seismic station can deliver essential flood metrics such as magnitude, propagation velocity and debris transport rate. These seismic products provide high resolution insight to the non‐linear flood behavior. We argue that an approach combining distributed low‐cost seismometers with existing seismic stations, can provide important real time data on future catastrophic floods and associated hazards in upland catchments, offering precious response time also in currently ungauged landscapes.
    Description: Plain Language Summary: Rapidly evolving floods are a major hazard for 10% of European landscapes. They are hard to adequately detect and describe by the classic gauge station scheme, but seismic sensors provide a valuable alternative to this difficulty. A seismometer can sense a flood like the devastating one that hit the Ahr valley, Germany, in July 2021 up to 1.5 km away. The seismic footprint of the flood allows to provide information on flood magnitude, velocity and trajectory at sub‐minute resolution and at near real time. We show how this new approach can be utilized for future flood protection.
    Description: Key Points: Seismic sensing of valley confined floods improves classic detection approaches. Near‐real time information on flood magnitude, trajectory, and velocity. Gate keeper seismometer networks can improve flood risk management in Europe.
    Description: GFZ German Research Centre for Geosciences
    Description: Helmholtz Centre Potsdam—GFZ German Research Centre for Geosciences http://dx.doi.org/10.13039/501100010956
    Description: German Research Foundation
    Keywords: ddc:622.1592 ; hazard ; realtime warning ; flash flood ; seismic
    Language: English
    Type: doc-type:article
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  • 3
    Publication Date: 2013-08-31
    Description: During the Galileo spacecraft encounter with the Earth-Moon system in December, 1992, a variety of spectral data and imagery were obtained for the eastern limb region as well as much of the lunar nearside. In order to support this encounter, we have been collecting near-infrared spectra and other remote sensing data for that portion of the northeastern nearside (NEM region) for which the highest resolution Galileo data were obtained. Analysis of spectra obtained for highlands units in the NEN region indicates that most surface units are dominated by anorthositic norite. To date, no pure anorthosites have been identified in the region. Several dark-haloed impact craters have exposed mare material from beneath highlands-rich surface units. Hence, ancient mare volcanism occurred in at least a portion of the NEN region. Endogenic dark-haloed craters in the region are the source of localized dark mantle deposits (LDMD) of pyroclastic origin and at least two compositional groups are present. The Galileo spacecraft obtained very high-resolution remote sensing data for the northeastern part of the nearside of the Moon. In order to prepare for and support this encounter, we have collected and analyzed a variety of spectral data for the NEN region. Numerous unanswered questions exist for this region. These include: (1) the composition and stratigraphy of the local highlands crust, (2) the nature and mode of formation of regional light plains, (3) the composition of localized pyroclastic deposits, and (4) the distribution of possible cryptomare in the region. The purpose of this paper is to present the preliminary results of our analyzes of remote sensing data of remote sensing data obtained for the NEN region.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: Lunar and Planetary Inst., Twenty-Fourth Lunar and Planetary Science Conference. Part 2: G-M; p 617-618
    Format: application/pdf
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  • 4
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    In:  Other Sources
    Publication Date: 2018-06-08
    Keywords: Lunar and Planetary Science and Exploration
    Type: Asteroid Rendezvous: NEAR Shoemaker's Adventures at Eros, Chapter 8
    Format: text
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  • 5
    Publication Date: 2021-07-01
    Description: In regions experiencing multiple phases of extension, rift‐related strain can vary along and across the basin during and between each phase, and the location of maximum extension can differ between the rift phase. Despite having a general understanding of multiphase rift kinematics, it remains unclear why the rift axis migrates between extension episodes. The role pre‐existing structures play in influencing fault and basin geometries during later rifting events is also poorly understood. We study the Stord Basin, northern North Sea, a location characterised by strain migration between two rift episodes. To reveal and quantify the rift kinematics, we interpreted a dense grid of 2D seismic reflection profiles, produced time‐structure and isochore (thickness) maps, collected quantitative fault kinematic data and calculated the amount of extension (β‐factor). Our results show that the locations of basin‐bounding fault systems were controlled by pre‐existing crustal‐scale shear zones. Within the basin, Permo‐Triassic Rift Phase 1 (RP1) faults mainly developed orthogonal to the E‐W extension direction. Rift faults control the locus of syn‐RP1 deposition, whilst during the inter‐rift stage, areas of clastic wedge progradation are more important in controlling sediment thickness trends. The calculated amount of RP1 extension (β‐factor) for the Stord Basin is up to β = 1.55 (±10%, 55% extension). During the subsequent Middle Jurassic‐Early Cretaceous Rift Phase 2 (RP2), however, strain localised to the west along the present axis of the South Viking Graben, with the Stord Basin being almost completely abandoned. Rift axis migration during RP2 is interpreted to be related to changes in lithospheric strength profile, possibly related to the ultraslow extension (〈1 mm/year during RP1), the long period of tectonic quiescence (ca. 50 myr) between RP1 and RP2 and possible underplating. Our results highlight the very heterogeneous nature of temporal and lateral strain migration during and between extension phases within a single rift basin.
    Description: Norges Forskningsråd http://dx.doi.org/10.13039/501100005416
    Keywords: 551.8 ; crustal extension ; multirifted basin ; Northern North Sea ; seismic interpretation ; tectonics and sedimentation
    Type: article
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  • 6
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    In:  Canad. J. Earth Sci., Warszawa, Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 36, no. 1, pp. 47-64, pp. 2121
    Publication Date: 1999
    Keywords: Induced seismicity ; Modelling ; Source ; Stress
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  • 7
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    In:  Earth planet. Sci. Lett., Beijing, Pergamon, vol. 45, no. 1, pp. 475-482, pp. 2135
    Publication Date: 1979
    Keywords: Stress ; Stress measurements ; Borehole breakouts
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  • 8
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    In:  Terra Nova, Beijing, Pergamon, vol. 7, no. 6, pp. 500-508, pp. 2135
    Publication Date: 1995
    Keywords: Tectonics ; Geol. aspects
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  • 9
    Publication Date: 1998
    Description: Precariously balanced boulders that could be knocked down by strong earthquake ground motion are found in some seismically active areas of southern California and Nevada. In this study we used two independent surface-exposure dating techniques - rock-varnish microlamination and cosmogenic 36Cl dating methodologies - to estimate minimum- and maximum-limiting ages, respectively, of the precarious boulders and by inference the elapsed time since the sites were shaken down. The results of the exposure dating indicate that all of the precarious rocks are 〉10.5 ka and that some may be significantly older. At Victorville and Jacumba, California, these results show that the precarious rocks have not been knocked down for at least 10.5 k.y., a conclusion in apparent conflict with some commonly used probabilistic seismic hazard maps. At Yucca Mountain, Nevada, the ages of the precarious rocks are 〉10.5 to 〉27.0 ka, providing an independent measure of the minimum time elapsed since faulting occurred on the Solitario Canyon fault.
    Keywords: Geol. aspects ; paleo ; Seismicity
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  • 10
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    In:  Canad. J. Earth Sci., University of Iceland, Icelandic Meteorological Office, Ministry for the Environment,, vol. 18, no. 4, pp. 638-645, pp. 1567, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1981
    Keywords: Stress ; cracks and fractures (.NE. fracturing) ; Borehole geophys.
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