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Do migratory flight paths of raptors follow constant geographical or geomagnetic courses? Do migratory flight paths of raptors follow constant geographical or geomagnetic courses?

We tested whether routes of raptors migrating over areas with homogeneous topography follow constant geomagnetic courses more or less closely than constant geographical courses. We analysed the routes taken over land of 45 individual raptors tracked by satellite-based radiotelemetry: 25 peregrine falcons, Falco peregrinus, on autumn migration between North and South America, and seven...
Authors
K. Thorup, M. Fuller, T. Alerstam, M. Hake, N. Kjellen, R. Strandberg

Spatial patterns of fish communities along two estuarine gradients in southern Florida Spatial patterns of fish communities along two estuarine gradients in southern Florida

In tropical and subtropical estuaries, gradients of primary productivity and salinity are generally invoked to explain patterns in community structure and standing crops of fishes. We documented spatial and temporal patterns in fish community structure and standing crops along salinity and nutrient gradients in two subtropical drainages of Everglades National Park, USA. The Shark River...
Authors
D.P.J. Green, J.C. Trexler, J.J. Lorenz, C.C. McIvor, T. Philippi

An effective medium inversion algorithm for gas hydrate quantification and its application to laboratory and borehole measurements of gas hydrate-bearing sediments An effective medium inversion algorithm for gas hydrate quantification and its application to laboratory and borehole measurements of gas hydrate-bearing sediments

The presence of gas hydrate in marine sediments alters their physical properties. In some circumstances, gas hydrate may cement sediment grains together and dramatically increase the seismic P- and S-wave velocities of the composite medium. Hydrate may also form a load-bearing structure within the sediment microstructure, but with different seismic wave attenuation characteristics...
Authors
S. Chand, T.A. Minshull, J.A. Priest, A.I. Best, C.R.I. Clayton, W.F. Waite

Ground deformation associated with the precursory unrest and early phases of the January 2006 eruption of Augustine volcano, Alaska Ground deformation associated with the precursory unrest and early phases of the January 2006 eruption of Augustine volcano, Alaska

On January 11, 2006 Augustine Volcano erupted after nearly 20 years of quiescence. Global Positioning System (GPS) instrumentation at Augustine, consisting of six continuously recording, telemetered receivers, measured clear precursory deformation consistent with a source of inflation or pressurization beneath the volcano's summit at a depth of around sea level. Deformation began in...
Authors
P.F. Cervelli, T. Fournier, Jeffrey T. Freymueller, J.A. Power

Volcanic history and 40Ar/39Ar and 14C geochronology of Terceira Island, Azores, Portugal Volcanic history and 40Ar/39Ar and 14C geochronology of Terceira Island, Azores, Portugal

Seven new 40Ar/39Ar and 23 new radiocarbon ages of eruptive units, in support of new geologic mapping, improve the known chronology of Middle to Late Pleistocene and Holocene volcanic activity on the island of Terceira, Azores and define an east-to-west progression in stratovolcano growth. The argon ages indicate that Cinco Picos Volcano, the oldest on Terceira, completed its main...
Authors
Andrew T. Calvert, Richard B. Moore, John P. McGeehin, Antonio Rodrigues da Silva

High-resolution stratigraphy of a Mississippi subdelta-lobe progradation in the Barataria Bight, north-central Gulf of Mexico High-resolution stratigraphy of a Mississippi subdelta-lobe progradation in the Barataria Bight, north-central Gulf of Mexico

The coastal zone of southeastern Louisiana is the product of numerous cycles of progradation, abandonment, and marine transgression of the Mississippi River delta. Currently, the shoreline in the Barataria Bight is undergoing significant erosion and retreat, and understanding its evolution is crucial in stabilization efforts. This study uses an extensive collection of geophysical and...
Authors
J. G. Flocks, N.F. Ferina, C. Dreher, J. L. Kindinger, D. M. FitzGerald, M.A. Kulp

Sensor web enables rapid response to volcanic activity Sensor web enables rapid response to volcanic activity

Rapid response to the onset of volcanic activity allows for the early assessment of hazard and risk [Tilling, 1989]. Data from remote volcanoes and volcanoes in countries with poor communication infrastructure can only be obtained via remote sensing [Harris et al., 2000]. By linking notifications of activity from ground-based and spacebased systems, these volcanoes can be monitored when...
Authors
Ashley G. Davies, Steve Chien, Robert Wright, Asta Mikijus, Philip R. Kyle, Matt Welsh, Jeffrey B. Johnson, Daniel Tran, Steven R. Schaffer, Robert Sherwood

Evaluating a small footprint, waveform-resolving lidar over coastal vegetation communities Evaluating a small footprint, waveform-resolving lidar over coastal vegetation communities

NASA’s Experimental Advanced Airborne Research Lidar (EAARL) is a raster-scanning, waveform-resolving, green-wavelength (532 nm) lidar designed to map near-shore bathymetry, topography, and vegetation structure simultaneously. The EAARL sensor records the time history of the return waveform within a small footprint (20 cm diameter) for each laser pulse, enabling characterization of...
Authors
Amar Nayegandhi, John Brock, C. Wayne Wright, M. J. O’Connell

Landslides caused by the M 7.6 Tecomán, Mexico earthquake of January 21, 2003 Landslides caused by the M 7.6 Tecomán, Mexico earthquake of January 21, 2003

The Tecomán, Mexico earthquake (also called the “Colima earthquake”) of January 21, 2003 (M 7.6) triggered several hundreds of landslides in the coastal cordilleras of Colima State, near the earthquake source, and several thousands in the volcanic highlands north and northwest of Colima City. These landslides, mostly shallow and disrupted failures, caused minor damage to roads, to a...
Authors
David K. Keefer, Joseph Wartman, Ochoa C. Navarro, Adrian Rodriguez-Marek, Gerald F. Wieczorek

Peak flow responses to landscape disturbances caused by the cataclysmic 1980 eruption of Mount St. Helens, Washington Peak flow responses to landscape disturbances caused by the cataclysmic 1980 eruption of Mount St. Helens, Washington

Years of discharge measurements that precede and follow the cataclysmic 1980 eruption of Mount St. Helens, Washington, provide an exceptional opportunity to examine the responses of peak flows to abrupt, widespread, devastating landscape disturbance. Multiple basins surrounding Mount St. Helens (300–1300 km2 drainage areas) were variously disturbed by: (1) a debris avalanche that buried...
Authors
Jon J. Major, Linda E. Mark

EAARL topography: Dry Tortugas National Park EAARL topography: Dry Tortugas National Park

This lidar-derived submarine topography map was produced as a collaborative effort between the U.S. Geological Survey (USGS) Coastal and Marine Geology Program, National Park Service (NPS) South Florida/Caribbean Network Inventory and Monitoring Program, and the National Aeronautics and Space Administration (NASA) Wallops Flight Facility. One objective of this research is to create...
Authors
John Brock, C. Wayne Wright, Matt Patterson, Amar Nayegandhi, Judd Patterson

Cartography for lunar exploration: 2006 status and planned missions Cartography for lunar exploration: 2006 status and planned missions

The initial spacecraft exploration of the Moon in the 1960s–70s yielded extensive data, primarily in the form of film and television images, that were used to produce a large number of hardcopy maps by conventional techniques. A second era of exploration, beginning in the early 1990s, has produced digital data including global multispectral imagery and altimetry, from which a new...
Authors
Randolph L. Kirk, Brent A. Archinal, Lisa R. Gaddis, Mark R. Rosiek
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