Conifers, incluing ponderosa pines, can be seen along the north rim of the Grand Canyon.
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Conifers, incluing ponderosa pines, can be seen along the north rim of the Grand Canyon.
A meniscus is seen along the edges of this glass cylinder.
A meniscus is seen along the edges of this glass cylinder.What is a meniscus?
A meniscus is a curve in the surface of a molecular substance (water, of course) when it touches another material. With water, you can think of it as when water sticks to the inside of a glass.
Why a meniscus occurs
A meniscus is seen along the edges of this glass cylinder.
A meniscus is seen along the edges of this glass cylinder.What is a meniscus?
A meniscus is a curve in the surface of a molecular substance (water, of course) when it touches another material. With water, you can think of it as when water sticks to the inside of a glass.
Why a meniscus occurs
Caribou with Calves during Summer in Northern Alaska
Caribou with Calves during Summer in Northern AlaskaCaribou with calves from the Central Arctic Herd in the Kuparuk Oil Field, Alaska.
Caribou with Calves during Summer in Northern Alaska
Caribou with Calves during Summer in Northern AlaskaCaribou with calves from the Central Arctic Herd in the Kuparuk Oil Field, Alaska.
Paper clip can float on water, due to high surface tension of water
Paper clip can float on water, due to high surface tension of waterIt seems to defy the laws of physics, but a paper clip made of steel can indeed float on the water surface. The high surface tension helps the paper clip - with much higher density - float on the water.
Paper clip can float on water, due to high surface tension of water
Paper clip can float on water, due to high surface tension of waterIt seems to defy the laws of physics, but a paper clip made of steel can indeed float on the water surface. The high surface tension helps the paper clip - with much higher density - float on the water.
USGS intern Kira Waldman collecting water-quality samples
USGS intern Kira Waldman collecting water-quality samplesEach summer, interns join USGS offices around the Nation in support of our water studies.
USGS intern Kira Waldman collecting water-quality samples
USGS intern Kira Waldman collecting water-quality samplesEach summer, interns join USGS offices around the Nation in support of our water studies.
Data locations for Ice Island Arctic Ocean Heat Flow Studies
Data locations for Ice Island Arctic Ocean Heat Flow StudiesData locations for Ice Island Arctic Ocean Heat Flow Studies
Data locations for Ice Island Arctic Ocean Heat Flow Studies
Data locations for Ice Island Arctic Ocean Heat Flow StudiesData locations for Ice Island Arctic Ocean Heat Flow Studies
Different portions of the ponds have different colors, presumably reflecting dif
Different portions of the ponds have different colors, presumably reflecting difDifferent portions of the ponds have different colors, presumably reflecting different amounts or varying chemistry of dissolved particles in the water.
Different portions of the ponds have different colors, presumably reflecting dif
Different portions of the ponds have different colors, presumably reflecting difDifferent portions of the ponds have different colors, presumably reflecting different amounts or varying chemistry of dissolved particles in the water.
Three SCREE hikers traversing a thin hiking trail to the saddle that separates the two arms of the Green River that defines the Bowknot Bend at Mile 63.
Three SCREE hikers traversing a thin hiking trail to the saddle that separates the two arms of the Green River that defines the Bowknot Bend at Mile 63.
magnified zircon crystal showing crystal growth age dating Yellowstone
magnified zircon crystal showing crystal growth age dating YellowstoneSections of a zircon crystal, only 100 micrometers across, showing stages of the crystal's growth. Upper panel shows the outer surface of the crystal, which is 131,000 years old based on 238U-230Th dating. This is when the crystal stopped growing. Lower panel shows the interior of the same zircon crystal.
magnified zircon crystal showing crystal growth age dating Yellowstone
magnified zircon crystal showing crystal growth age dating YellowstoneSections of a zircon crystal, only 100 micrometers across, showing stages of the crystal's growth. Upper panel shows the outer surface of the crystal, which is 131,000 years old based on 238U-230Th dating. This is when the crystal stopped growing. Lower panel shows the interior of the same zircon crystal.
Title: USGS Fire Science: Understanding why wildlands burn and what can be done about it
Title: USGS Fire Science: Understanding why wildlands burn and what can be done about it
Schematic diagram of Yellowstone's current magmatic system.
Schematic diagram of Yellowstone's current magmatic system.Schematic diagram of Yellowstone's current magmatic system. A silicic crystal-mush (gray region with white crystals) is thought to underlie the caldera at a depth of ~5 km to 15 km, with more mafic basalt (in black) underneath.
Schematic diagram of Yellowstone's current magmatic system.
Schematic diagram of Yellowstone's current magmatic system.Schematic diagram of Yellowstone's current magmatic system. A silicic crystal-mush (gray region with white crystals) is thought to underlie the caldera at a depth of ~5 km to 15 km, with more mafic basalt (in black) underneath.
Taken from the saddle, a panoramic view of the Bowknot Bend of the Green River. The Bowknot Bend is 7 river miles around. Erosion will eventually shorten the river course considerably.
Taken from the saddle, a panoramic view of the Bowknot Bend of the Green River. The Bowknot Bend is 7 river miles around. Erosion will eventually shorten the river course considerably.
The California Aqueduct flowing near Huron, CA in the San Joaquin Valley. This spot is near one of several USGS land subsidence monitoring stations in the San Joaquin Valley.
The California Aqueduct flowing near Huron, CA in the San Joaquin Valley. This spot is near one of several USGS land subsidence monitoring stations in the San Joaquin Valley.
On behalf of the Hawaiian Volcano Observatory, Carolyn Donlin, Chief of the USGS Menlo Park Publishing Service Center, accepted an award from the National Association of Government Communicators recognizing HVO's weekly "Volcano Watch" articles as excellent communication products.
On behalf of the Hawaiian Volcano Observatory, Carolyn Donlin, Chief of the USGS Menlo Park Publishing Service Center, accepted an award from the National Association of Government Communicators recognizing HVO's weekly "Volcano Watch" articles as excellent communication products.
Four recently hatched piping plover chicks huddle in the nest bowl
Four recently hatched piping plover chicks huddle in the nest bowlFour recently hatched piping plover chicks huddle in the nest bowl on the Garrison Reach of the Missouri River, North Dakota
Four recently hatched piping plover chicks huddle in the nest bowl
Four recently hatched piping plover chicks huddle in the nest bowlFour recently hatched piping plover chicks huddle in the nest bowl on the Garrison Reach of the Missouri River, North Dakota
Sampling Big Sandy River below Farson, WY
Collecting water samples for eDNA analysis to estimate foothill yellow
Collecting water samples for eDNA analysis to estimate foothill yellowUSGS technicians collect water samples for eDNA analysis to estimate foothill yellow-legged frog (Rana boylii) presence at historically occupied sites throughout Oregon. These data are important for assessing the species' status and conservation needs.
Collecting water samples for eDNA analysis to estimate foothill yellow
Collecting water samples for eDNA analysis to estimate foothill yellowUSGS technicians collect water samples for eDNA analysis to estimate foothill yellow-legged frog (Rana boylii) presence at historically occupied sites throughout Oregon. These data are important for assessing the species' status and conservation needs.
This image from a viewpoint at Dead Horse State Park in Utah shows horizontal Mesozoic sedimentary rocks characteristic of the Colorado Plateau. The Colorado River can be seen from this vantage point and this state park is located between Canyonlands National Park to the southwest and Arches National Park to the northeast.
This image from a viewpoint at Dead Horse State Park in Utah shows horizontal Mesozoic sedimentary rocks characteristic of the Colorado Plateau. The Colorado River can be seen from this vantage point and this state park is located between Canyonlands National Park to the southwest and Arches National Park to the northeast.
At about Mile 102 you can see Dellenbaugh Butte, which is also known as The Anvil, or Inkwell Butte. Powell camped here July 14, 1869. The majority of the butte is composed of the Summerville Formation.
At about Mile 102 you can see Dellenbaugh Butte, which is also known as The Anvil, or Inkwell Butte. Powell camped here July 14, 1869. The majority of the butte is composed of the Summerville Formation.
Female Southwestern Willow Flycatcher with colorful bands
Female Southwestern Willow Flycatcher with colorful bandsFemale Southwestern Willow Flycatcher with colorful bands in 2019 on the upper San Luis Rey River. The bird was originally banded as a nestling by USGS biologist Scarlett Howell on the upper San Luis Rey River in July 2017.
Female Southwestern Willow Flycatcher with colorful bands
Female Southwestern Willow Flycatcher with colorful bandsFemale Southwestern Willow Flycatcher with colorful bands in 2019 on the upper San Luis Rey River. The bird was originally banded as a nestling by USGS biologist Scarlett Howell on the upper San Luis Rey River in July 2017.
Qu'est-ce que le cycle de l'eau?