Beach loss and armoring at Goleta Beach, very low (negative) tide
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Images related to natural hazards.
Beach loss and armoring at Goleta Beach, very low (negative) tide
This image comparison shows the changing nature of the lava stream ...
This image comparison shows the changing nature of the lava stream ...This image comparison shows the changing nature of the lava stream between Saturday, January 28 and Wednesday, February 1. The lava stream has become much more narrow, as viewed from this angle.
This image comparison shows the changing nature of the lava stream ...
This image comparison shows the changing nature of the lava stream ...This image comparison shows the changing nature of the lava stream between Saturday, January 28 and Wednesday, February 1. The lava stream has become much more narrow, as viewed from this angle.
Bedrock exposed at low tide along the beach at Isla Vista, California
Bedrock exposed at low tide along the beach at Isla Vista, California
From the lava viewing area established by Hawai‘i Volcanoes Nationa...
From the lava viewing area established by Hawai‘i Volcanoes Nationa...From the lava viewing area established by Hawai‘i Volcanoes National Park, you can witness Kīlauea Volcano's ocean entry from a safe distance. With binoculars or a telephoto camera lens, spectacular views and photos are possible (as seen here)—without risking your life by entering the closed area.
From the lava viewing area established by Hawai‘i Volcanoes Nationa...
From the lava viewing area established by Hawai‘i Volcanoes Nationa...From the lava viewing area established by Hawai‘i Volcanoes National Park, you can witness Kīlauea Volcano's ocean entry from a safe distance. With binoculars or a telephoto camera lens, spectacular views and photos are possible (as seen here)—without risking your life by entering the closed area.
Using a telephoto lens, spatter and glassy rock fragments (black sa...
Using a telephoto lens, spatter and glassy rock fragments (black sa...Using a telephoto lens, spatter and glassy rock fragments (black sand) from the explosive interaction of molten lava and seawater can be seen flying skyward and seaward. At times, these fragments were thrown high enough to land on the sea cliff above the ocean entry—one of many hazards impacting this area.
Using a telephoto lens, spatter and glassy rock fragments (black sa...
Using a telephoto lens, spatter and glassy rock fragments (black sa...Using a telephoto lens, spatter and glassy rock fragments (black sand) from the explosive interaction of molten lava and seawater can be seen flying skyward and seaward. At times, these fragments were thrown high enough to land on the sea cliff above the ocean entry—one of many hazards impacting this area.
The hot crack near the sea cliff, in the immediate area of the ocean entry, has widened significantly over the past four days. On Saturday, January 28, the crack was 30 cm wide (1 foot). Today, HVO geologists in protective gear briefly entered the area and measured the crack as being 75 cm (2.5 feet).
The hot crack near the sea cliff, in the immediate area of the ocean entry, has widened significantly over the past four days. On Saturday, January 28, the crack was 30 cm wide (1 foot). Today, HVO geologists in protective gear briefly entered the area and measured the crack as being 75 cm (2.5 feet).
Ground crack at Kīlauea ocean entry is cause for concern
Ground crack at Kīlauea ocean entry is cause for concernDue to the instability of the sea cliff above the ocean entry and other hazards created by molten lava flowing into the sea, Hawai‘i Volcanoes National Park has established a viewing area (noted by yellow arrow in photo) from which the ocean entry can be seen in relative safety.
Ground crack at Kīlauea ocean entry is cause for concern
Ground crack at Kīlauea ocean entry is cause for concernDue to the instability of the sea cliff above the ocean entry and other hazards created by molten lava flowing into the sea, Hawai‘i Volcanoes National Park has established a viewing area (noted by yellow arrow in photo) from which the ocean entry can be seen in relative safety.
A wider view of the ocean entry, at sunset.
A wider view of the ocean entry, at sunset.
Carefully approaching the site in protective gear on Jan. 28, Geolo...
Carefully approaching the site in protective gear on Jan. 28, Geolo...Carefully approaching the site in protective gear on Jan. 28, HVO geologists determined that the eastern end of the hot crack was about 30 cm (11.8 in) wide and deeply cut into recent lava atop the older sea cliff. The western end could not be accessed due to poor air quality, spatter fallout, and other safety concerns.
Carefully approaching the site in protective gear on Jan. 28, Geolo...
Carefully approaching the site in protective gear on Jan. 28, Geolo...Carefully approaching the site in protective gear on Jan. 28, HVO geologists determined that the eastern end of the hot crack was about 30 cm (11.8 in) wide and deeply cut into recent lava atop the older sea cliff. The western end could not be accessed due to poor air quality, spatter fallout, and other safety concerns.
the open lava stream pouring into ocean. Frequent littoral explosi...
the open lava stream pouring into ocean. Frequent littoral explosi...This video clip shows the open lava stream pouring into the ocean. Frequent littoral explosions throw bits of lava to heights of over 27 m (30 yards).
the open lava stream pouring into ocean. Frequent littoral explosi...
the open lava stream pouring into ocean. Frequent littoral explosi...This video clip shows the open lava stream pouring into the ocean. Frequent littoral explosions throw bits of lava to heights of over 27 m (30 yards).
The lava stream, pouring out of the lava tube on the sea cliff at the Kamokuna ocean entry, continues and was similar to yesterday. The stream appeared wider (as viewed from this angle) today compared to yesterday, and often had holes in the thin sheet. The entry was still producing small, pulsating littoral explosions.
The lava stream, pouring out of the lava tube on the sea cliff at the Kamokuna ocean entry, continues and was similar to yesterday. The stream appeared wider (as viewed from this angle) today compared to yesterday, and often had holes in the thin sheet. The entry was still producing small, pulsating littoral explosions.
Using a thermal image of the crack above Kīlauea's ocean entry (ste...
Using a thermal image of the crack above Kīlauea's ocean entry (ste...Using a thermal image of the crack above Kīlauea volcano's ocean entry (steam from lava flowing into the sea is visible at the top of the left photo), HVO geologists determined that the temperature within the eastern end of the crack is up to about 220 degrees Celsius (428 degrees Fahrenheit).
Using a thermal image of the crack above Kīlauea's ocean entry (ste...
Using a thermal image of the crack above Kīlauea's ocean entry (ste...Using a thermal image of the crack above Kīlauea volcano's ocean entry (steam from lava flowing into the sea is visible at the top of the left photo), HVO geologists determined that the temperature within the eastern end of the crack is up to about 220 degrees Celsius (428 degrees Fahrenheit).
At Kīlauea's ocean entry on Jan. 28 and 29, the interaction of molt...
At Kīlauea's ocean entry on Jan. 28 and 29, the interaction of molt...At Kīlauea's ocean entry on Jan. 28 and 29, the interaction of molten lava flowing into cool seawater caused pulsating littoral explosions that threw spatter (fragments of molten lava) high into the air. Some of these incandescent clasts fell on top of the sea cliff behind the ocean entry, forming a small spatter cone.
At Kīlauea's ocean entry on Jan. 28 and 29, the interaction of molt...
At Kīlauea's ocean entry on Jan. 28 and 29, the interaction of molt...At Kīlauea's ocean entry on Jan. 28 and 29, the interaction of molten lava flowing into cool seawater caused pulsating littoral explosions that threw spatter (fragments of molten lava) high into the air. Some of these incandescent clasts fell on top of the sea cliff behind the ocean entry, forming a small spatter cone.
An open lava stream continues to pour out of the lava tube, perched high on the sea cliff, and into the ocean. The stream was remarkably steady today, but produced pulsating littoral explosions that threw spatter onto the sea cliff.
An open lava stream continues to pour out of the lava tube, perched high on the sea cliff, and into the ocean. The stream was remarkably steady today, but produced pulsating littoral explosions that threw spatter onto the sea cliff.
base of the lava stream, where ripples in the narrow sheet of lava ...
base of the lava stream, where ripples in the narrow sheet of lava ...This video shows a close-up of the base of the lava stream, where ripples in the narrow sheet of lava are visible.
base of the lava stream, where ripples in the narrow sheet of lava ...
base of the lava stream, where ripples in the narrow sheet of lava ...This video shows a close-up of the base of the lava stream, where ripples in the narrow sheet of lava are visible.
A close up of the stream near spot where it exits the tube. This v...
A close up of the stream near spot where it exits the tube. This v...A close up of the stream near the spot where it exits the tube. This view was only possible with a very high magnification lens.
A close up of the stream near spot where it exits the tube. This v...
A close up of the stream near spot where it exits the tube. This v...A close up of the stream near the spot where it exits the tube. This view was only possible with a very high magnification lens.
A wider view of the ocean entry.
A wider view of the ocean entry.
Near the base of the lava stream, just above where it impacted the ...
Near the base of the lava stream, just above where it impacted the ...Near the base of the lava stream, just above where it impacted the water, there were commonly ripples in the stream, suggesting this was a narrow sheet of lava. These ripples can be seen on the lower right side of the lava stream. A few small, steaming clasts thrown up by a small littoral explosion are visible in front of the stream.
Near the base of the lava stream, just above where it impacted the ...
Near the base of the lava stream, just above where it impacted the ...Near the base of the lava stream, just above where it impacted the water, there were commonly ripples in the stream, suggesting this was a narrow sheet of lava. These ripples can be seen on the lower right side of the lava stream. A few small, steaming clasts thrown up by a small littoral explosion are visible in front of the stream.
open lava stream at the ocean entry, and the frequent littoral expl...
open lava stream at the ocean entry, and the frequent littoral expl...This video shows a wider view of the open lava stream at the ocean entry, and the frequent littoral explosions.
open lava stream at the ocean entry, and the frequent littoral expl...
open lava stream at the ocean entry, and the frequent littoral expl...This video shows a wider view of the open lava stream at the ocean entry, and the frequent littoral explosions.
HVO geophysicist shares information at a public outreach event for ...
HVO geophysicist shares information at a public outreach event for ...HVO geophysicist shares information at a public outreach event for Volcano Awareness Month at the University of Hawai‘i at Hilo in January 2017.
HVO geophysicist shares information at a public outreach event for ...
HVO geophysicist shares information at a public outreach event for ...HVO geophysicist shares information at a public outreach event for Volcano Awareness Month at the University of Hawai‘i at Hilo in January 2017.
Exploring USGS volcano observatories—Part 4: Yellowstone
Exploring USGS volcano observatories—Part 4: YellowstoneYellowstone National Park is the site of Earth's largest concentration of geysers, as well as steam vents, hot springs, and mudpots. These hydrothermal features attest to the region's volcanic history, which spans over two million years and is the reason that the Yellowstone Volcano Observatory was established.
Exploring USGS volcano observatories—Part 4: Yellowstone
Exploring USGS volcano observatories—Part 4: YellowstoneYellowstone National Park is the site of Earth's largest concentration of geysers, as well as steam vents, hot springs, and mudpots. These hydrothermal features attest to the region's volcanic history, which spans over two million years and is the reason that the Yellowstone Volcano Observatory was established.