Image showing MTL contour, marsh edge, and example of calculating the marsh edge
Images
Image showing MTL contour, marsh edge, and example of calculating the marsh edge
![A boat floating on calm, shallow waters with mountains far off in the distance.](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/Fault1DeploymentBoatOnSeaofGalilee.jpg?itok=W5ut6WQr)
The Israel Oceanographic and Limnological Institute research boat Lillian on its way to deploy receivers in the Sea of Galilee to record data during an April, 2018 experiment to image the deep structure of the Dead Sea fault in Israel.
The Israel Oceanographic and Limnological Institute research boat Lillian on its way to deploy receivers in the Sea of Galilee to record data during an April, 2018 experiment to image the deep structure of the Dead Sea fault in Israel.
One of 40 seismic receivers modified to work in water and anchored to the bottom of the Sea of Galilee in Israel's Dead Sea fault zone.
One of 40 seismic receivers modified to work in water and anchored to the bottom of the Sea of Galilee in Israel's Dead Sea fault zone.
Working in a temporary lab in Kibbutz Moran, Lloyd Carothers (left, IRIS-PASSCAL) and Eldad Levi (Geophysical Institute of Israel) download data from seismic receivers (in blue and yellow boxes) retrieved after completion of the Dead Sea fault experiment.
Working in a temporary lab in Kibbutz Moran, Lloyd Carothers (left, IRIS-PASSCAL) and Eldad Levi (Geophysical Institute of Israel) download data from seismic receivers (in blue and yellow boxes) retrieved after completion of the Dead Sea fault experiment.
![In background, photo shows a view of a beach with hotels and skyscrapers along the shore, text advertisement on top.](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/Apr18flyer-pg1.jpg?itok=6JvDbq9e)
Flyer to advertise the upcoming USGS Menlo Park Campus Free Public Lecture on April 26, 2018: "The Role of U.S.
Flyer to advertise the upcoming USGS Menlo Park Campus Free Public Lecture on April 26, 2018: "The Role of U.S.
USGS geomorphologist Pat Limber drives an all-terrain vehicle equipped with differential GPS, on Ellwood Beach in Goleta, California, collecting topographic, or elevation and contour, data. These data, accurate to about 1 inch (about 2 centimeters) both horizontally and vertically, are used to monitor seasonal beach changes.
USGS geomorphologist Pat Limber drives an all-terrain vehicle equipped with differential GPS, on Ellwood Beach in Goleta, California, collecting topographic, or elevation and contour, data. These data, accurate to about 1 inch (about 2 centimeters) both horizontally and vertically, are used to monitor seasonal beach changes.
Jackson Currie of the USGS Pacific Coastal and Marine Science Center drives a personal watercraft (PWC) offshore of Butterfly Beach in Montecito, California. The equipment on the PWC collects bathymetry, or depth, data which is used to map the nearshore. USGS has been mapping this area twice yearly—every spring and fall—since 2005.
Jackson Currie of the USGS Pacific Coastal and Marine Science Center drives a personal watercraft (PWC) offshore of Butterfly Beach in Montecito, California. The equipment on the PWC collects bathymetry, or depth, data which is used to map the nearshore. USGS has been mapping this area twice yearly—every spring and fall—since 2005.
USGS volunteer Josh Brown on Santa Claus Beach, Carpinteria, at the start of a 14-mile walking survey of southern California beaches. The differential GPS equipment carried in the backpack collects elevation, or topographic, data of the beach, accurate to about 1 inch (2 centimeters) both horizontally and vertically.
USGS volunteer Josh Brown on Santa Claus Beach, Carpinteria, at the start of a 14-mile walking survey of southern California beaches. The differential GPS equipment carried in the backpack collects elevation, or topographic, data of the beach, accurate to about 1 inch (2 centimeters) both horizontally and vertically.
USGS geomorphologist Pat Limber drives an all-terrain vehicle equipped with differential GPS, on San Buenaventura Beach south of Ventura Pier, Ventura California, collects topographic, or elevation and contour, data. These data, accurate to about 1 inch (about 2 centimeters) both horizontally and vertically, are used to monitor seasonal beach changes.
USGS geomorphologist Pat Limber drives an all-terrain vehicle equipped with differential GPS, on San Buenaventura Beach south of Ventura Pier, Ventura California, collects topographic, or elevation and contour, data. These data, accurate to about 1 inch (about 2 centimeters) both horizontally and vertically, are used to monitor seasonal beach changes.
Jackson Currie and Alex Snyder of the USGS Pacific Coastal and Marine Science Center drive personal watercraft (PWCs) offshore of San Ysidro and Oak Creeks, which let out onto Miramar Beach in Montecito, California.
Jackson Currie and Alex Snyder of the USGS Pacific Coastal and Marine Science Center drive personal watercraft (PWCs) offshore of San Ysidro and Oak Creeks, which let out onto Miramar Beach in Montecito, California.
Two USGS scientists operate personal watercraft equipped with sonar and GPS along the beachfront off San Ysidro Creek, near Fernald Point in Montecito, California. They will use the data collected to create bathymetric (depth) maps.
Two USGS scientists operate personal watercraft equipped with sonar and GPS along the beachfront off San Ysidro Creek, near Fernald Point in Montecito, California. They will use the data collected to create bathymetric (depth) maps.
Footprints in mud layer deposited on the sand at Miramar Beach in Montecito, California, by January 9 flood waters coming down San Ysidro Creek.
Footprints in mud layer deposited on the sand at Miramar Beach in Montecito, California, by January 9 flood waters coming down San Ysidro Creek.
Shruti Khanna (left, California Department of Fish and Wildlife) and Judy Drexler (USGS California Water Science Center) on the USGS Pacific Coastal and Marine Science Center’s research vessel Parke Snavely during fieldwork in the Sacramento-San Joaquin River Delta.
Shruti Khanna (left, California Department of Fish and Wildlife) and Judy Drexler (USGS California Water Science Center) on the USGS Pacific Coastal and Marine Science Center’s research vessel Parke Snavely during fieldwork in the Sacramento-San Joaquin River Delta.
Patches of dark sand cling to an instrument package that collected data for approximately two weeks at the Mokelumne River site—evidence that currents at the site were strong enough to carry sand, which is heavier than mud, probably during elevated river flows following two storms in the watershed.
Patches of dark sand cling to an instrument package that collected data for approximately two weeks at the Mokelumne River site—evidence that currents at the site were strong enough to carry sand, which is heavier than mud, probably during elevated river flows following two storms in the watershed.
Drone image of Nauset Inlet, Cape Cod National Seashore, Massachusetts
Drone image of Nauset Inlet, Cape Cod National Seashore, Massachusetts
Dive Safety Officer (DSO) Jake Emmert from Moody Gardens Aquarium enters a flooded coastal cave beneath the tropical forest of the Yucatan Peninsula through a small open-water pool, locally known as a cenote. Cave diving scientists John Pohlman (USGS) and David Brankovits (USGS/WHOI) will use these entrances over the coming days to access a vast network o
Dive Safety Officer (DSO) Jake Emmert from Moody Gardens Aquarium enters a flooded coastal cave beneath the tropical forest of the Yucatan Peninsula through a small open-water pool, locally known as a cenote. Cave diving scientists John Pohlman (USGS) and David Brankovits (USGS/WHOI) will use these entrances over the coming days to access a vast network o
USGS physical scientist Cordell Johnson, at left, and USGS research oceanographer Jessie Lacy, both from the Pacific Coastal and Marine Science Center, guide a tripod with instruments into the waters of the Mokelumne River near the confluence with the San Joaquin River. The Mokelumne is part of the vast Sacramento-San Joaquin River Delta in California,&nbs
USGS physical scientist Cordell Johnson, at left, and USGS research oceanographer Jessie Lacy, both from the Pacific Coastal and Marine Science Center, guide a tripod with instruments into the waters of the Mokelumne River near the confluence with the San Joaquin River. The Mokelumne is part of the vast Sacramento-San Joaquin River Delta in California,&nbs
Dan Powers (USGS PCMSC) and Rachel Marcuson (USGS PCMSC) prepare to deploy a Gomex sediment corer from the R/V Snavely in the Mokulumne River near confluence of San Joaquin River in the Sacramento-San Joaquin Delta, CA.
Dan Powers (USGS PCMSC) and Rachel Marcuson (USGS PCMSC) prepare to deploy a Gomex sediment corer from the R/V Snavely in the Mokulumne River near confluence of San Joaquin River in the Sacramento-San Joaquin Delta, CA.
![A man is leaning over and is scooping soil from a wildfire-charred hillslope and placing the soil in a sample bag.](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/Ro_NorCalSoilMar18LG.jpg?itok=bWhIUI32)
Brett Tipple (University of California, Santa Cruz) collects a sample of charcoal and soil adjacent to a gully forming on a hillslope above Sonoma Creek, which was burned by the Nuns wildfire in October 2017.
Brett Tipple (University of California, Santa Cruz) collects a sample of charcoal and soil adjacent to a gully forming on a hillslope above Sonoma Creek, which was burned by the Nuns wildfire in October 2017.
John Pohlman (USGS), David Brankovits (USGS/WHOI) and Jake Emmert (MG) deploy acoustic devices in open water sinkhole (or cenote) prior to a 6-month long installation in the Yucatan Peninsula, Mexico cave
John Pohlman (USGS), David Brankovits (USGS/WHOI) and Jake Emmert (MG) deploy acoustic devices in open water sinkhole (or cenote) prior to a 6-month long installation in the Yucatan Peninsula, Mexico cave
The remnants of an eroding marsh sit on a bayside beach behind Long Beach Island, New Jersey. Marsh loss and bayside erosion can be outcomes of both natural landscape evolution and human modification of coastal barrier systems.
The remnants of an eroding marsh sit on a bayside beach behind Long Beach Island, New Jersey. Marsh loss and bayside erosion can be outcomes of both natural landscape evolution and human modification of coastal barrier systems.