Results 181 to 190 of about 9,726 (207)
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Late Quaternary distal tephra-fall deposits in lacustrine sediments, Kenai Peninsula, Alaska
Quaternary Research, 2007AbstractTephra-fall deposits from Cook Inlet volcanoes were detected in sediment cores from Tustumena and Paradox Lakes, Kenai Peninsula, Alaska, using magnetic susceptibility and petrography. The ages of tephra layers were estimated using 21 14C ages on macrofossils.
Christian S. de Fontaine +5 more
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Bulletin of Volcanology, 1992
A model for sedimentation from turbulent suspensions predicts that tephra concentration decreases exponentially with time in an ascending volcanic column and in the overlying umbrella cloud. For grain-size distributions typical of plinian eruptions application of the model predicts for thickness variations in good agreement with the exponential ...
Sparks, RSJ +4 more
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A model for sedimentation from turbulent suspensions predicts that tephra concentration decreases exponentially with time in an ascending volcanic column and in the overlying umbrella cloud. For grain-size distributions typical of plinian eruptions application of the model predicts for thickness variations in good agreement with the exponential ...
Sparks, RSJ +4 more
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Geochemical and geotechnical characterization of compacted air-fall tephras
2023Presentation by University of Canterbury PhD student Shaurya ...
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Probabilistic tephra fall simulation for the Auckland Region, New Zealand
Journal of Volcanology and Geothermal Research, 2006Abstract The Auckland Region, New Zealand is at significant risk from tephra falls originating both from the local Auckland Volcanic Field (AVF) and several distant, large-volume centres. We use geological data and observations of historical eruptions to develop a catalogue of simulated tephra dispersal patterns for the Auckland Region, using the ...
C.R. Magill +3 more
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A model for the numerical simulation of tephra fall deposits
Journal of Volcanology and Geothermal Research, 2005Abstract A simple semianalytical model to simulate ash dispersion and deposition produced by sustained Plinian and sub-Plinian eruption columns based on the 2D advection–dispersion equation was applied. The eruption column acts as a vertical line source with a given mass distribution and neglects the complex dynamics within the eruption column. Thus,
T. Pfeiffer, A. Costa, G. Macedonio
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Forest fire following Holocene tephra fall
1981The rhyolitic eruptions of the Taupo Pumice (c. 1800 B.P.) and the Kaharoa Ash (c. 700 B.P.) devastated forest close to the volcanic source. However, pollen diagrams from regions up to 150 km from the volcanic centre show that widespread fires were common over an appreciable period after both eruptions.
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Some Effects of Tephra Falls on Buildings
1981A survey of the volcanological literature reveals that only limited generalisations concerning the effects of volcanic bomb impacts and tephra loads on buildings can be made. By using data from a variety of other sources, however, it is possible to define the impact energies required to penetrate or damage a variety of building materials.
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Agricultural vulnerability to tephra fall impacts.
2015Understanding agricultural impact from tephra hazards and their causal mechanisms is vital when developing mitigation and recovery strategies. It is well documented that tephra can impact agricultural systems. However, forecasting likely impacts has been challenging and focused on creating generalised models where impacts typically increase with tephra
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Combined effects of wind and column mass distribution on tephra fall deposits
Environmental Software, 1990Abstract A 2D1/2 model of volcanic ashes (tephra) dispersion, based on an analytical solution of the advection-diffusion equation, is presented. By this model the correlation between a double maximum in thickness and a punctual bimodal size distribution in plinian deposit of volcanic eruptions is outlined for the first time.
P. Armienti, G. Macedonio, M.T. Pareschi
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A varve-based calibration of the Bridge River tephra fall
Canadian Journal of Earth Sciences, 1995A 1 cm thick layer of Bridge River tephra is preserved in a core of varved lake sediments recovered from Hector Lake, Alberta. The varve sequence extends from the core top to well below the tephra layer and has bseen calibrated to calendar years. A varve count yields a calendar age of 2332 BP for the ash layer, with a potential error of about ±50 ...
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