Some media are reporting that the Asian H5N1 strain of highly pathogenic avian influenza has now entered the United States. This is incorrect. The avian flu that was recently found in a green-winged teal in Washington state is a different strain and is not known to harm humans nor has it been found in domestic poultry. This Washington state strain incorporates genes from North American waterfowl-associated viruses. Unlike the Asian H5N1 strain that has been found in Asia, Europe, and Africa, this Washington state strain has only been found in wild waterfowl and has not been associated with human illness, nor has this new Washington state strain been found in domestic poultry.
Catherine Puckett, USGS ( Phone: 352-377-2469 );
BOZEMAN – Pallid sturgeon come from a genetic line that has lived on this planet for tens of millions of years; yet it has been decades since anyone has documented any of the enormous fish successfully producing young that survive to adulthood in the upper Missouri River basin.
Now, fisheries scientists with the U.S. Geological Survey, Montana State University and the U.S. Fish and Wildlife Service have shown why, detailing for the first time the biological mechanism that has caused the long decline of pallid sturgeon in the Missouri River and led to its being placed on the endangered species list 25 years ago.
In a paper published this week in the journal Fisheries, the scientists show that oxygen-depleted dead zones between dams in the upper Missouri River are directly linked with the failure of endangered pallid sturgeon hatched embryos to survive to adulthood.
“This research is a notable breakthrough in identifying the reason why pallid sturgeon in the Missouri River have been declining for so many decades,” said Suzette Kimball, acting director of the USGS. “By pinpointing the biological mechanism responsible for the species’ decline, resource managers have vital information they can use as a focus of pallid sturgeon conservation.”
“We certainly think this is a significant finding in the story of why pallid sturgeon are failing to recruit in the upper Missouri River,” said Christopher Guy, the assistant unit leader with the USGS Montana Cooperative Fishery Research Unit and the MSU professor who was the lead author on the paper. “We’re basically talking about a living dinosaur that takes 20 years to reach sexual maturity and can live as long as the average human in the U.S. After millions of years of success, the pallid sturgeon population stumbled and now we know why. From a conservation perspective, this is a major breakthrough.”
The study is the first to make a direct link among dam-induced changes in riverine sediment transport, the subsequent effects of those changes on reduced oxygen levels and the survival of an endangered species, the pallid sturgeon.
“This research shows that the transition zone between the freely flowing river and reservoirs is an ecological sink – a dead zone – for pallid sturgeon,” Guy said. “Essentially, hatched sturgeon embryos die in the oxygen-depleted sediments in the transition zones.”
Guy said fisheries biologists long suspected that the Missouri River’s massive reservoirs were preventing hatched embryonic pallid sturgeon from surviving to the juvenile stage. But early attempts to tie the problem to low levels of dissolved oxygen were unsuccessful.
“The reason for that is we hadn’t sampled deep enough,” Guy said. “It wasn’t until we sampled water down at the bottom, where those sediments are being deposited, that we found there was no dissolved oxygen. Because hatched pallid sturgeon embryos are negatively buoyant, they tend to sink into that hostile environment.”
“The lack of oxygen is a function of high microbial activity in the sediment laden area,” said co-author Eric Scholl, a Ph.D. student at Montana State University and a co-author on the study.
Hilary Treanor, an MSU research associate working with Guy, said they were able to show just how hostile these transition zones between riverine environment and reservoir could be to hatched sturgeon embryos.
In experiments at the U.S. Fish and Wildlife Fish Technology Center in Bozeman with coauthors Molly Webb, Kevin Kappenman, and Jason Ilgen, Treanor said different aged hatched embryos were treated with water of varying levels of dissolved oxygen. The lowest level they could recreate – 1.5 milligrams of oxygen per liter of water – was still higher than samples pulled from the bottom at the upper end of Fort Peck Reservoir.
At those depleted levels, the hatched sturgeon embryos suffered almost immediately.
“We saw changes in their behavior fairly quickly. They became disoriented and weren’t able to move the way they should have,” Treanor said. “Within an hour we started to see mortality. By the end of the experiment they were all dead.”
"Pallid sturgeon, native to the Missouri and Mississippi rivers, were listed as an endangered species in 1990. The species has a lifespan of as much as a century. According to the U.S. Fish and Wildlife Service, fewer than 175 wild-spawned pallid sturgeon – all adults – live in the free-flowing Missouri River above Lake Sakakawea. Since 1990, not a single wild-spawned pallid sturgeon is known to have survived to a juvenile, despite intensive searching.
In the past 5 years, researchers identified the most important reason for pallid sturgeon population declines in the Upper Missouri River: the lack of survival of naturally produced hatched sturgeon embryos.
Guy said this most recent study of sturgeon built on research conducted by USGS fisheries biologist Patrick Braaten, which demonstrated not enough available drift distance exists between the reservoirs for hatched pallid sturgeon embryos before entering the reservoirs in the upper Missouri River.
Before dams, hatched pallid sturgeon embryos would drift for hundreds of miles, eventually settling out of the river’s current in areas with low flow where they matured enough to negotiate the river’s flow.
“This team has shown how much we can do when we have a collaboration between MSU, USGS and world-renowned reproductive physiologists Molly Webb and Kevin Kappenman with the U.S. Fish and Wildlife Service,” Guy said. “In the process of doing this research, we’ve trained a dozen MSU graduate students and a number of undergraduate field and lab techs.”
Given what the new research shows about how no oxygen is available to hatched pallid sturgeon embryos, the authors of the paper propose that officials will need to consider innovative approaches to managing Missouri River reservoirs for pallid sturgeon conservation to have a chance. It also could provide some guiding principles for the construction of new dams around the world, Guy said.
EATONTOWN, N.J. -- In the two years and three months since Hurricane Sandy scored a direct hit on New Jersey, the Federal Emergency Management Agency has remained engaged in the recovery effort, providing $6.9 billion to date to help the state recover and rebuild.Language English
SPOKANE, Wash. — In cooperation with the Polish Geological Institute — National Research Institute, U.S. Geological Survey scientists have published a new assessment of copper resources in Poland and Germany. This investigation is part of the U.S. Geological Survey’s Global Mineral Resource Assessment. The study synthesizes available information on known resources and estimates the location and quantity of undiscovered copper associated with the well-known late Permian (approximately 255 million years old), carbon-enriched shale, the Kupferschiefer, of the Southern Permian Basin in Europe.
The ore deposits associated with the Kupferschiefer in Germany and Poland have been mined for over 800 years and are world-famous among geologists because research on these deposits played a significant role in the scientific debates on ore genesis. The largest Kupferschiefer copper deposit occurs in the Lubin-Sieroszowice mining area, Poland. It is the largest copper deposit in Europe and one of the largest copper deposits on the Earth.
Most of the known copper resource and almost all of the estimated undiscovered copper resources occur in southwestern Poland and adjacent parts of eastern Germany. Since 1958, about 15 million metric tons of copper have been produced, and about 30 million metric tons of discovered copper remains to be developed. The USGS estimates a mean value of 110 million metric tons of copper may be undiscovered to a depth of 2.5 km below the surface in this area. Most of the undiscovered resource in southwestern Poland would be deeper than 1.5 km, where virgin rock temperatures exceed 50 degrees C (122 degrees F).
In 800 years of mining, about 2.6 million metric tons of copper were produced from Kupferschiefer deposits in east-central Germany. The areas near the deposits in east-central Germany have been well explored; less than one million metric tons of discovered copper remain in identified deposits. Mean undiscovered copper estimates for this area are about 20 million metric tons.
This USGS study supports previous findings by the Polish Geological Institute for the amount of undiscovered copper in Poland. Mean values from the USGS study are remarkably similar to the values estimated by Polish geologists. The USGS study differs from the Polish study in that two different methods are used to probabilistically estimate the amount of undiscovered copper and maps are included to show where undiscovered resources are likely to occur.
The full report, USGS Scientific Investigations Report 2010–5090–U, “Assessment of undiscovered copper resources associated with the Permian Kupferschiefer, Southern Permian Basin, Europe,” by Michael Zientek and others, is available online.
Additional USGS mineral resource assessment results and reports, including previous volumes of this publication series, and an estimate of undiscovered copper resource of the world in 2013, are online.
The U.S. Geological Survey (USGS) has released a convenient and informative new method for the analysis of groundwater and surface-water hydrologic data called the Groundwater (GW) Toolbox. The GIS-driven graphical and mapping interface is a significant advancement in USGS software for estimating base flow (the groundwater-discharge component of streamflow), surface runoff, and groundwater recharge from streamflow data.
The GW Toolbox brings together several analysis methods previously developed by the USGS and Bureau of Reclamation. Each of the methods included with the GW Toolbox use daily streamflow data automatically retrieved from the USGS National Water Information System (NWIS) for more than 26,000 streamgage sites across the United States. In addition to streamflow data, the GW Toolbox facilitates the retrieval of groundwater-level and precipitation time-series data from the NWIS database.
The GW Toolbox will be of use to engineers, academia, and government agencies at all levels for the analysis of many of the water-budget components of a typical watershed. The intensively visual interface will help shed light on water availability and hydrologic trends in response to climate and land-use changes and variability in these watersheds.
The GW Toolbox runs in a Microsoft Windows environment and includes the Base Flow Index (BFI), HYSEP, and PART hydrograph-separation methods to estimate base flow and surface runoff and the RORA and RECESS methods to estimate groundwater recharge.
WASHINGTON – The Federal Emergency Management Agency (FEMA) today announced it is seeking applicants for its Youth Preparedness Council. The Council supports FEMA’s commitment to involving youth in preparedness-related activities and provides an opportunity for young people to offer their perspectives, feedback and insights on how to help make America more resilient.Language English
WASHINGTON – The U.S. Department of Homeland Security’s Federal Emergency Management Agency (FEMA) seeks experienced individuals who are interested in serving on the National Advisory Council (NAC) to apply. All applications must be received by 5 p.m. ET on Monday, February 16, 2015.Language English
ANCHORAGE, Alaska Melting glaciers are not just impacting sea level, they are also affecting the flow of organic carbon to the world’s oceans, according to new research that provides the first ever global-scale estimates for the storage and release of organic carbon from glaciers.
The research, published in the Jan. 19 issue of Nature Geoscience, is crucial to better understand the role glaciers play in the global carbon cycle, especially as climate warming continues to reduce glacier ice stores and release ice-locked organic carbon into downstream freshwater and marine ecosystems.
“This research makes it clear that glaciers represent a substantial reservoir of organic carbon,” said Eran Hood, the lead author on the paper and a scientist with the University of Alaska Southeast (Juneau). “As a result, the loss of glacier mass worldwide, along with the corresponding release of carbon, will affect high-latitude marine ecosystems, particularly those surrounding the major ice sheets that now receive fairly limited land-to-ocean fluxes of organic carbon.”
Polar ice sheets and mountain glaciers cover roughly 11 percent of the Earth’s land surface and contain about 70 percent of Earth’s fresh water. They also store and release organic carbon to downstream environments as they melt. Because this glacier-derived organic carbon is readily metabolized by microorganisms, it can affect productivity in aquatic ecosystems.
“This research demonstrates that the impacts of glacier change reach beyond sea level rise,” said U.S. Geological Survey research glaciologist and co-author of the research Shad O’Neel. “Changes in organic carbon release from glaciers have implications for aquatic ecosystems because this material is readily consumed by microbes at the bottom of the food chain.”
Due to climate change, glacier mass losses are expected to accelerate, leading to a cumulative loss of nearly 17 million tons of glacial dissolved organic carbon by 2050 — equivalent to about half of the annual flux of dissolved organic carbon from the Amazon River.
These estimates are the first of their kind, and thus have high uncertainty, the scientists wrote, noting that refining estimates of organic carbon loss from glaciers is critical for improving the understanding of the impacts of glacier change. The U.S. Department of the Interior Alaska Climate Science Center and USGS Alaska Science Center plan to continue this work in 2015 and beyond with new efforts aimed at studying the biophysical implications of glacier change.
This project highlights ongoing collaboration between academic and federal research and the transformative results that stem from such funding partnerships. Other institutions involved in the research include Ecole Polytechnique Fédérale de Lausanne and Florida State University.
The work was supported by the National Science Foundation, the USGS Alaska Science Center, and the DOI Alaska Climate Science Center. The Alaska Climate Science Center provides scientific information to help natural resource managers and policy makers respond effectively to climate change.
ATLANTA–Preliminary flood insurance rate maps for Sarasota County, Fla., can be reviewed at three public open houses during the week of January 19, 2015. Flood maps show the extent to which areas are at risk for flooding, and are used to help determine flood insurance and building requirements.Language English
SEATTLE – As Washingtonians deal with the aftermath of severe storms and flooding that occurred a week ago, the recovery process may include a flood insurance claim. There are three steps to file a claim with the National Flood Insurance Program (NFIP):
- Contact your insurance agent.
- Document your damaged property.
- File a Proof of Loss form within 60 days of the flood.
More details are available at www.FloodSmart.gov.Language English
Newly released US Topo maps for Nebraska now feature trails provided to the USGS through a “crowdsourcing” project operated by the International Mountain Biking Association (IMBA). Several of the 1,376 new US Topo quadrangles for the state now display trails along with other improved data layers such as map symbol redesign and new road source data.
"As an avid cyclist I look forward to exploring the new US Topo maps for bike trails as I plan my trips," said Jim Langtry, National Map Liaison for Nebraska. "I look forward to the expansion of the trail network and hope this encourages the crowdsourcing effort to add and maintain trails for future updates. It would be great to see the Cowboy Trail, the nation’s longest rails-to-trail trek along the northern tier of Nebraska, included on the next update. You can hike, bike, or horseback ride a total of 195 miles on the completed trail from Norfolk to Valentine. Enjoy the small towns along the way, beautiful scenery and pristine air on the Cowboy Trail."
For Nebraska residents and visitors who want to explore the rolling “cornhusker” landscape on a bicycle seat, the new trail features on the US Topo maps will come in handy. The data is provided through a partnership with IMBA and MTB Project. During the past two years, the IMBA has been building a detailed national database of mountain bike trails with the aid and support of the MTB Project. This activity allows local IMBA chapters, IMBA members, and the public to provide trail data and descriptions through their website. MTB Project and IMBA then verify the quality of the trail data provided, ensure accuracy and confirm that the trail is legal. This unique crowdsourcing venture has increased the availability of trail data available through The National Map mobile and web apps, and the revised US Topo maps.
These new maps replace the first edition US Topo maps for Nebraska and are available for free download from The National Map, the USGS Map Locator & Downloader website , or several other USGS applications.
To compare change over time, scans of legacy USGS topo maps, some dating back to the late 1800s, can be downloaded from the USGS Historical Topographic Map Collection
For more information on US Topo maps: http://nationalmap.gov/ustopo/New version of the North Platte, Nebraska US Topo quadrangle: 2014, with orthoimage turned on. (1:24,000 scale) (high resolution image 1.2 MB) 1902 historic version of the North Platte, Nebraska US Topo quadrangle at 1;25,000 scale. (high resolution image 1.8 MB)
VANCOUVER, Wash. — The large landslide that occurred on March 22, 2014 near Oso, Washington was unusually mobile and destructive. The first published study from U.S. Geological Survey investigations of the Oso landslide (named the “SR530 Landslide” by Washington State) reveals that the potential for landslide liquefaction and high mobility are influenced by several factors, and the landslide process at Oso could have unfolded very differently (with much less destruction) if initial conditions had been only subtly different.
A major focus of the research reported this week is to understand the causes and effects of the landslide’s high mobility. High “mobility” implies high speeds and large areas of impact, which can be far from the landslide source area. Because high-mobility landslides overrun areas that are larger than normal, they present a significant challenge for landslide hazard evaluation. Understanding of the Oso event adds to the knowledge base that can be used to improve future hazard evaluations.
Computer reconstructions of the landslide source-area geometry make use of high-resolution digital topographic (lidar) data, and they indicate that the Oso landslide involved about 8 million cubic meters (about 18 million tons, or almost 3 times the mass of the Great Pyramid of Giza) of material. The material consisted of sediments deposited by ancient glaciers and in streams and lakes near the margins of those glaciers. The landslide occurred after a long period of unusually wet weather. Prolonged wet weather increases groundwater pressures, which act to destabilize slopes by reducing frictional resistance between sediment particles.
The slope that failed at Oso on March 22, 2014 had a long history of prior historical landslides at the site, but these had not exhibited exceptional mobility.
The area overrun by the March 22 landslide was about 1.2 square kilometers (one-half square mile), mostly on the nearly flat floodplain of the North Fork Stillaguamish River. Additional areas were affected by upstream flooding along the river, which was partially dammed by the landslide. Eyewitness accounts and seismic energy radiated by the landslide indicate that slope failure occurred in two stages over the course of about 1 minute. During the second stage of slope failure, the landslide greatly accelerated, crossed the North Fork Stillaguamish River, and mobilized to form a high-speed debris avalanche. The leading edge of the wet debris avalanche probably acquired additional water as it crossed the North Fork Stillaguamish River. It transformed into a water-saturated debris flow (a fully liquefied slurry of quicksand-like material) that entrained and transported virtually all objects in its path.
Field evidence and mathematical modeling indicate that the high mobility of the debris avalanche was caused by liquefaction at the base of the slide caused by pressures generated by the landslide itself. The physics of landslide liquefaction has been studied experimentally and is well understood, but the complex nature of natural geological materials complicates efforts to predict which landslides will liquefy and become highly mobile.
Results from a suite of computer simulations indicate that the landslide’s liquefaction and high mobility were very sensitive to its initial porosity and water content. Landslide mobility may have been far less if the landslide material had been slightly denser and/or drier. Computer simulations that best fit field observations and seismological interpretations indicate that the fast-moving landslide crossed the entire 1-km-wide river floodplain in about one minute, implying an average speed of about 40 miles per hour. Maximum speeds were even higher.
Only one individual landslide in U.S. history (an event in Mameyes, Puerto Rico in 1985 that killed at least 129) caused more fatalities than the 43 that occurred in the 2014 landslide near Oso.
The full paper, “Landslide mobility and hazards: implications of the 2014 Oso disaster” by R.M. Iverson et al. is published in the journal, “Earth and Planetary Science Letters” and is freely available online.Oso landslide simulation screen shot. (High resolution image) (Video)
[Access images for this release at: &amp;amp;amp;lt;a href="http://gallery.usgs.gov/tags/NR2015_01_12" _mce_href="http://gallery.usgs.gov/tags/NR2015_01_12"&amp;amp;amp;gt;http://gallery.usgs.gov/tags/NR2015_01_12&amp;amp;amp;lt;/a&amp;amp;amp;gt;]
Following is a summary of key federal disaster aid programs that can be made available as needed and warranted under President Obama’s major disaster declaration issued for Mississippi.
Assistance for the State and Affected Local Governments Can Include as Required:Language English
WASHINGTON, D.C. – The U.S. Department of Homeland Security's Federal Emergency Management Agency announced that federal disaster aid has been made available to the state of Mississippi to supplement state and local recovery efforts in the area affected by severe storms and tornadoes on December 23, 2014.Language English
DENTON, Texas – Homeowners, renters and business owners in El Paso County in Texas are encouraged to look over newly-revised preliminary flood maps in order to determine their flood risks and make informed decisions.Language English
DENTON, Texas– Months of teamwork by officials from Dona Ana County and the Federal Emergency Management Agency (FEMA) have led to new preliminary flood maps. Now, the public is encouraged to participate in a 90-day appeal and comment period about the maps.
Homeowners, renters and business owners in Dona Ana County are encouraged to view the preliminary flood maps to better understand where flood risks have been identified. Those who would like to file an appeal have until March 11, 2015 to submit them.Language English
Newly released US Topo maps for Arizona now feature mountain bike trails, segments of the Arizona National Scenic Trail and Public Land Survey System data. Several of the 1,880 new US Topo quadrangles for the state now display these selected new features along with other improved data layers.
“Having recently returned to Arizona, I am excited to re-explore our state using the new USGS Arizona Topo maps,” said Curtis Pulford, Arizona State Cartographer. “Detailed topographic maps are one of the best ways I know to visualize the terrain one is planning to examine. All who use these will appreciate the newly updated reference features, such as BLM Public Lands Survey System, roadways, schools, fire and police stations, post offices, and hospitals. Mountain bikers will appreciate the addition of International Mountain Biking Association trails. And the addition of the 817 mile, border to border, Arizona National Scenic Trail will be an outstanding resource for nature enthusiasts, hikers and equestrians.”
For Arizona residents and visitors who want to explore the landscape on a bicycle seat, the new mountain bike trails will come in handy. The mountain bike trail data is provided through a partnership with the International Mountain Biking Association (IMBA) and MTB Project. During the past two years, the IMBA has been building a detailed national database of mountain bike trails with the aid and support of the MTB Project. This activity allows local IMBA chapters, IMBA members, and the public to provide trail data and descriptions through their website. MTB Project and IMBA then verify the quality of the trail data provided, ensure accuracy and confirm that the trail is legal. This unique “crowdsourcing” project has allowed availability of mountain bike trail data though mobile and web apps, and the revised US Topo maps.
National Scenic Trail enthusiasts can now find the “Arizona Trail” on new US Topo map segments. The Arizona National Scenic Trail stretches more than 800 miles from the Mexican border to Utah to connect deserts, mountains, canyons, wilderness, history, communities and people. Rugged, wild and challenging, this trail showcases Arizona’s diverse vegetation, wildlife, scenery, and historic and prehistoric sites in a way that provides a unique and unparalleled Arizona experience.
“For more than 20 years the Arizona Trail Association’s members have been creating, maintaining, and mapping the Arizona National Scenic Trail,” said Aaron Seifert, GIS Director for the Arizona Trail Association. “Since the trail was designated as a National Scenic Trail in 2009 and completed in 2011, it is very exciting to display the entire trail on the new set of US Topo maps for many more to discover the diverse landscape of Arizona from this amazing trail.”
The USGS partnered with the U.S. Forest Service and the Arizona Trail Association to incorporate the trail data onto the Arizona US Topo maps. This NST joins the Ice Age National Scenic Trail, the Pacific Northwest National Scenic Trail the North Country National Scenic Trail, the Pacific Crest National Scenic Trail, and the Appalachian National Scenic Trail as being featured on the new US Topo quads. The USGS hopes to eventually include all National Scenic Trails in The National Map products.
Another important addition to the new Arizona US Topo maps in the inclusion of Public Land Survey System. PLSS is a way of subdividing and describing land in the US. All lands in the public domain are subject to subdivision by this rectangular system of surveys, which is regulated by the U.S. Department of the Interior.
These new maps replace the first edition US Topo maps for Arizona and are available for free download from The National Map, the USGS Map Locator & Downloader website , or several other USGS applications.
To compare change over time, scans of legacy USGS topo maps, some dating back to the late 1800s, can be downloaded from the USGS Historical Topographic Map Collection
For more information on US Topo maps: http://nationalmap.gov/ustopo/New (2014) Black Canyon City, Arizona US Topo quadrangle with orthoimage turn on. (1:24,000 scale). (high resolution image 1.3 MB) Historical USGS topographic map of the Prescott, Arizona area (1887). !:250,000 scale. (high resolution image 1.6 MB) Zoom of the Black Canyon City, Arizona, US Topo quadrangle. The Blank Canyon Trail (BCT) is denoted by a dashed line on the left side of the graphic. (high resolution image 1.2 MB)
Heidi Koontz ( Phone: 303-202-4763 );
While the number of large earthquakes fell to 12 in 2014, from 19 in 2013, several moderate temblors hit areas relatively new to seismicity, including Oklahoma and Kansas, according to the U.S. Geological Survey. Worldwide, 11 earthquakes reached magnitude 7.0-7.9 and one registered magnitude 8.2, in Iquique, Chile, on April 1. This is the lowest annual total of earthquakes magnitude 7.0 or greater since 2008, which also had 12.
Earthquakes were responsible for about 664 deaths in 2014, with 617 having perished in the magnitude 6.1 Ludian Xian, Yunnan, China, event on August 3, as reported by the United Nations Office for Coordination of Humanitarian Affairs. Deadly quakes also occurred in Chile, Nicaragua, Papua New Guinea, and the United States.
A magnitude 6.0 quake struck American Canyon, California (South Napa) in the early hours of August 24, triggering more than 41,300 responses via the USGS Did You Feel It? website. One woman died from her injuries 12 days later. This temblor also represents northern California’s strongest earthquake since the October 1989 Loma Prieta event.
The biggest earthquake in the United States, and the second largest quake of 2014, was a magnitude 7.9 event in the Aleutian Islands of Alaska on June 23. Several quakes below magnitude 5.0 rattled Oklahoma, Texas, Kansas, Arkansas and Arizona throughout the year. The USGS estimates that several million earthquakes occur throughout the world each year, although most go undetected because they have very small magnitudes or hit remote areas.
On average, the USGS National Earthquake Information Center (NEIC) publishes the locations for about 40 earthquakes per day, or about 14,500 annually. The USGS NEIC publishes worldwide earthquakes with a magnitude of 4.0 or greater or U.S. earthquakes of 2.5 or greater. On average each year since about 1900, 18 have a magnitude of 7.0 or higher.
To monitor earthquakes worldwide, the USGS NEIC receives data in real-time from about 1,700 stations in more than 90 countries. These stations include the 150-station Global Seismographic Network, which is jointly supported by the USGS and the National Science Foundation, and is operated by the USGS in partnership with the Incorporated Research Institutions for Seismology (IRIS) consortium of universities. Domestically, the USGS partners with 13 regional seismic networks operated by universities that provide detailed coverage for the areas of the country with the highest seismic risk.
In the U.S., 42 of the 50 states, plus Puerto Rico, may experience damaging ground shaking from an earthquake in 50 years, the nominal lifetime of a building. The USGS and its partners in the multi-agency National Earthquake Hazard Reduction Program are working to improve earthquake monitoring and reporting capabilities through the development of the USGS Advanced National Seismic System (ANSS). More information about ANSS can be found on the ANSS website.
Read a USGS feature story to learn more about other natural hazards in 2014.
Paul Laustsen ( Phone: 650-329-4046 );
Editors: B-roll footage of polar bear research is available for your use.
ANCHORAGE, Alaska — In a new polar bear study published today, scientists from around the Arctic have shown that recent generations of polar bears are moving towards areas with more persistent year-round sea ice.
Research scientists, led by the U.S. Geological Survey, found that the 19 recognized subpopulations of polar bears group into four genetically-similar clusters, corresponding to ecological and oceanographic factors. These four clusters are the Eastern Polar Basin, Western Polar Basin, Canadian Archipelago, and Southern Canada.
The scientists also detected directional gene flow towards the Canadian Archipelago within the last 1-3 generations. Gene flow of this type can result from populations expanding and contracting at different rates or directional movement and mating over generations. The findings of spatial structure (clusters) and directional gene flow are important because they support the hypothesis that the species is coalescing to the region of the Arctic most likely to retain sea ice into the future.
“The polar bear’s recent directional gene flow northward is something new,” said Elizabeth Peacock, USGS researcher and lead author of the study. “In our analyses that focused on more historic gene flow, we did not detect movement in this direction.” The study found that the predominant gene flow was from Southern Canada and the Eastern Polar Basin towards the Canadian Archipelago where the sea ice is more resilient to summer melt due to circulation patterns, complex geography, and cooler northern latitudes.
Projections of future sea ice extent in light of climate warming typically show greater retention of sea ice in the northern Canadian Archipelago than in other regions.
“By examining the genetic makeup of polar bears, we can estimate levels and directions of gene flow, which represents the past story of mating and movement, and population expansion and contraction,” said Peacock. “Gene flow occurs over generations, and would not be detectable by using data from satellite-collars which can only be deployed on a few polar bears for short periods of time.”
The authors also found that female polar bears showed higher fidelity to their regions of birth than did male polar bears. Data to allow comparison of the movements of male and female polar bears is difficult to obtain because male bears cannot be collared as their necks are wider than their heads.
The study also confirmed earlier work that suggests that modern polar bears stem from one or several hybridization events with brown bears. No evidence of current polar bear-brown bear hybridization was found in the more than 2,800 samples examined in the current study. Scientists concluded that the hybrid bears that have been observed in the Northern Beaufort Sea region of Canada represent a recent and currently localized phenomenon. Scientists also found that polar bear populations expanded and brown bear populations contracted in periods with more ice. In periods with less ice, the opposite was true.
The goal of the study was to see how genetic diversity and structure of the worldwide polar bear population have changed over the recent dramatic decline in their sea-ice habitat. The USGS and the Government of Nunavut led the study with scientists from 15 institutions representing all five nations with polar bears (U.S., Canada, Greenland, Norway, and Russia).
This circumpolar, multi-national effort provides a timely perspective on how a rapidly changing Arctic is influencing the gene flow and likely future distribution of a species of worldwide conservation concern.
The paper “Implications of the circumpolar genetic structure of polar bears for their conservation in a rapidly warming Arctic” was published today in the journal PLOS One.
CHICAGO – Dangerously low temperatures and accumulating snow are in the forecast for much of the Midwest and the U.S. Department of Homeland Security’s Federal Emergency Management Agency (FEMA) wants individuals and families to be safe when faced with the hazards of cold temperatures and winter weather.Language English