Publications
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The colonial ascidian Didemnum sp. A: current distribution, basic biology and potential threat to marine communities of the northeast and west coasts of North America The colonial ascidian Didemnum sp. A: current distribution, basic biology and potential threat to marine communities of the northeast and west coasts of North America
Didemnum sp. A is a colonial ascidian with rapidly expanding populations on the east and west coasts of North America. The origin of Didemum sp. A is unknown. Populations were first observed on the northeast coast of the U.S. in the late 1980s and on the west coast during the 1990s. It is currently undergoing a massive population explosion and is now a dominant member of many subtidal...
Authors
S.G. Bullard, G. Lambert, M.R. Carman, J. Byrnes, R.B. Whitlatch, G. Ruiz, R. J. Miller, L. Harris, P. C. Valentine, J.S. Collie, J. Pederson, D.C. McNaught, A.N. Cohen, R. G. Asch, J. Dijkstra, K. Heinonen
Swarms of repeating long-period earthquakes at Shishaldin Volcano, Alaska, 2001-2004 Swarms of repeating long-period earthquakes at Shishaldin Volcano, Alaska, 2001-2004
During 2001–2004, a series of four periods of elevated long-period seismic activity, each lasting about 1–2 months, occurred at Shishaldin Volcano, Aleutian Islands, Alaska. The time periods are termed swarms of repeating events, reflecting an abundance of earthquakes with highly similar waveforms that indicate stable, non-destructive sources. These swarms are characterized by increased
Authors
Tanja Petersen
Explosive eruptive record in the Katmai region, Alaska Peninsula: An overview Explosive eruptive record in the Katmai region, Alaska Peninsula: An overview
At least 15 explosive eruptions from the Katmai cluster of volcanoes and another nine from other volcanoes on the Alaska Peninsula are preserved as tephra layers in syn- and post-glacial (Last Glacial Maximum) loess and soil sections in Katmai National Park, AK. About 400 tephra samples from 150 measured sections have been collected between Kaguyak volcano and Mount Martin and from...
Authors
Judy Fierstein
Introduction--Subduction's sharpest arrow Introduction--Subduction's sharpest arrow
No abstract available.
Authors
J.C. Eichelberger
National volcanic ash operations plan for aviation National volcanic ash operations plan for aviation
The National Aviation Weather Program Strategic Plan (1997) and the National Aviation Weather Initiatives (1999) both identified volcanic ash as a high-priority informational need to aviation services. The risk to aviation from airborne volcanic ash is known and includes degraded engine performance (including flameout), loss of visibility, failure of critical navigational and operational
Authors
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Debris flow hazards mitigation--Mechanics, prediction, and assessment Debris flow hazards mitigation--Mechanics, prediction, and assessment
These proceedings contain papers presented at the Fourth International Conference on Debris-Flow Hazards Mitigation: Mechanics, Prediction, and Assessment held in Chengdu, China, September 10-13, 2007. The papers cover a wide range of topics on debris-flow science and engineering, including the factors triggering debris flows, geomorphic effects, mechanics of debris flows (e.g., rheology
Lava effusion rate definition and measurement: a review Lava effusion rate definition and measurement: a review
Measurement of effusion rate is a primary objective for studies that model lava flow and magma system dynamics, as well as for monitoring efforts during on-going eruptions. However, its exact definition remains a source of confusion, and problems occur when comparing volume flux values that are averaged over different time periods or spatial scales, or measured using different approaches...
Authors
Sonia Calvari, Jonathan Dehn, A. Harris
Sediment compaction rates and subsidence in deltaic plains: Numerical constraints and stratigraphic influences Sediment compaction rates and subsidence in deltaic plains: Numerical constraints and stratigraphic influences
Natural sediment compaction in deltaic plains influences subsidence rates and the evolution of deltaic morphology. Determining compaction rates requires detailed knowledge of subsurface geotechnical properties and depositional history, neither of which is often readily available. To overcome this lack of knowledge, we numerically forward model the incremental sedimentation and compaction...
Authors
T.A. Meckel, Uri S. ten Brink, S.J. Williams
Characterisation and modelling of washover fans Characterisation and modelling of washover fans
Pre- and post-storm topography and aerial photography, collected in regions where new washover fans were formed, were studied to determine the extent of morphologic, vegetative and anthropogenic control on washover shape and extent. When overwash is funnelled through a gap in a dune ridge and then spreads laterally on the back barrier, decelerating and depositing sediment, it forms...
Authors
Chantal Donnelly, Asbury H. Sallenger
A deep reef in deep trouble A deep reef in deep trouble
The well-documented degradation of shallower reefs which are often closer to land and more vulnerable to pollution, sewage and other human-related stressors has led to the suggestion that deeper, more remote offshore reefs could possibly serve as sources of coral and fish larvae to replenish the shallower reefs. Yet, the distribution, status, and ecological roles of deep (>30 m)...
Authors
Charles Menza, M. Kendall, C. Rogers, J. Miller
Sandy signs of a tsunami's onshore depth and speed Sandy signs of a tsunami's onshore depth and speed
Tsunamis rank among the most devastating and unpredictable natural hazards to affect coastal areas. Just 3 years ago, in December 2004, the Indian Ocean tsunami caused more than 225,000 deaths. Like many extreme events, however, destructive tsunamis strike rarely enough that written records span too little time to quantify tsunami hazard and risk. Tsunami deposits preserved in the...
Authors
K. Huntington, J. Bourgeois, G. Gelfenbaum, P. Lynett, B. Jaffe, H. Yeh, R. Weiss
Investigation of magnesium isotope fractionation during basalt differentiation: Implications for a chondritic composition of the terrestrial mantle Investigation of magnesium isotope fractionation during basalt differentiation: Implications for a chondritic composition of the terrestrial mantle
To investigate whether magnesium isotopes are fractionated during basalt differentiation, we have performed high-precision Mg isotopic analyses by multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS) on a set of well-characterized samples from Kilauea Iki lava lake, Hawaii, USA. Samples from the Kilauea Iki lava lake, produced by closed-system crystal-melt...
Authors
F.-Z. Teng, M. Wadhwa, Rosalind T. Helz