Kalapana Gardens subdivision inundated by pāhoehoe, Kīlauea
Kalapana Gardens subdivision inundated by pāhoehoe, KīlaueaKalapana Gardens subdivision inundated by pāhoehoe flows, Kīlauea Volcano, Hawai‘i
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Images related to natural hazards.
Kalapana Gardens subdivision inundated by pāhoehoe flows, Kīlauea Volcano, Hawai‘i
Kalapana Gardens subdivision inundated by pāhoehoe flows, Kīlauea Volcano, Hawai‘i
Lava flow moving into the town of Kalapana, Hawaii Island. Flow front is center, silver-black mass with rising fume. Buildings and lagoon in this photograph were completely buried within one month.
Lava flow moving into the town of Kalapana, Hawaii Island. Flow front is center, silver-black mass with rising fume. Buildings and lagoon in this photograph were completely buried within one month.
The left edge of the lava flow is following the inland contours of Hakuma horst, the fault block to the left, which is directing the flow into the heart of Kalapana.
The left edge of the lava flow is following the inland contours of Hakuma horst, the fault block to the left, which is directing the flow into the heart of Kalapana.
Harry K. Brown Park was originally called "Wai'akolea Park." It was renamed "Harry Ka'ina Brown Memorial Park" in 1953 after Brown, a county auditor, whose ancestral home was in Kalapana. Thick smoke is from burning asphalt.
Harry K. Brown Park was originally called "Wai'akolea Park." It was renamed "Harry Ka'ina Brown Memorial Park" in 1953 after Brown, a county auditor, whose ancestral home was in Kalapana. Thick smoke is from burning asphalt.
Lava flows in the upper center are moving toward the bottom of this photograph into the town of Kalapana, Hawaii. Today, all the vegetated and habited areas are paved by newer lava flows.
Lava flows in the upper center are moving toward the bottom of this photograph into the town of Kalapana, Hawaii. Today, all the vegetated and habited areas are paved by newer lava flows.
A three-story house in Kalapana Gardens is ignited by a lava flow, which entered the subdivision on April 17, 1990. By the 24th, more than a dozen houses were destroyed.
A three-story house in Kalapana Gardens is ignited by a lava flow, which entered the subdivision on April 17, 1990. By the 24th, more than a dozen houses were destroyed.
Ascending eruption cloud from Redoubt Volcano as viewed to the west from the Kenai Peninsula. The mushroom-shaped plume rose from avalanches of hot debris (pyroclastic flows) that cascaded down the north flank of the volcano. A smaller, white steam plume rises from the summit crater.
Ascending eruption cloud from Redoubt Volcano as viewed to the west from the Kenai Peninsula. The mushroom-shaped plume rose from avalanches of hot debris (pyroclastic flows) that cascaded down the north flank of the volcano. A smaller, white steam plume rises from the summit crater.
Aerial view of pāhoehoe flow encroaching on the Kalapana community. Hakuma horst, a raised fault block, is on the left. To the right of the point are fishponds, and to their right, Walter's Kalapana Store and Drive Inn. In the large trapezoidal plot are Mauna Kea Congregational Church and hall.
Aerial view of pāhoehoe flow encroaching on the Kalapana community. Hakuma horst, a raised fault block, is on the left. To the right of the point are fishponds, and to their right, Walter's Kalapana Store and Drive Inn. In the large trapezoidal plot are Mauna Kea Congregational Church and hall.
Dusting of Redoubt Volcano ash on snow, Indian, Alaska, February 21, 1990.
Dusting of Redoubt Volcano ash on snow, Indian, Alaska, February 21, 1990.
View looking uphill at surface flows advancing down a steep slope (Pulama pali) between the east rift zone and the coastal plain of Kīlauea Volcano. Overflows from the channel on the right are building levees of pāhoehoe. Within a few days, crust accreting inward from the levees built a roof over the channel, forming a new lava tube.
View looking uphill at surface flows advancing down a steep slope (Pulama pali) between the east rift zone and the coastal plain of Kīlauea Volcano. Overflows from the channel on the right are building levees of pāhoehoe. Within a few days, crust accreting inward from the levees built a roof over the channel, forming a new lava tube.
An automobile lies crushed under the third story of this apartment building in the Marina District. The ground levels are no longer visible because of structural failure and sinking due to liquefaction.
An automobile lies crushed under the third story of this apartment building in the Marina District. The ground levels are no longer visible because of structural failure and sinking due to liquefaction.
Top: Dark glassy deposits of melted volcanic ash on leading edge of highâ€pressure turbine nozzle guide vanes. Bottom: Accumulation of unmelted volcanic ash in the high-pressure turbine rotor.
Top: Dark glassy deposits of melted volcanic ash on leading edge of highâ€pressure turbine nozzle guide vanes. Bottom: Accumulation of unmelted volcanic ash in the high-pressure turbine rotor.
Lava flows from a lava tube into the sea near Kupapau Point on Hawai'i Island. From the Kilauea East Rift Zone (ERZ) eruption, November 27, 1989. Episode 48 of the Kupapau Lava Flow.
Lava flows from a lava tube into the sea near Kupapau Point on Hawai'i Island. From the Kilauea East Rift Zone (ERZ) eruption, November 27, 1989. Episode 48 of the Kupapau Lava Flow.
Lava flows from a lava tube into the sea near Kupapau Point on 11/27/1989. From the Kilauea East Rift Zone (ERZ) eruption, eruption pisode 48, Kupapau lava flow. Hawai'i Island.
Lava flows from a lava tube into the sea near Kupapau Point on 11/27/1989. From the Kilauea East Rift Zone (ERZ) eruption, eruption pisode 48, Kupapau lava flow. Hawai'i Island.
A downtown building at the corner of Alice and 13th Streets lost part of its unreinforced facade and brick masonry.
A downtown building at the corner of Alice and 13th Streets lost part of its unreinforced facade and brick masonry.
Pahoehoe ropes form in the Wahaula Lava Flow across from Wahaula Visitor Center on Hawai'i Island during the Kilauea East Rift Zone (ERZ) eruption on 6/15/89.
Pahoehoe ropes form in the Wahaula Lava Flow across from Wahaula Visitor Center on Hawai'i Island during the Kilauea East Rift Zone (ERZ) eruption on 6/15/89.
Sediment retention dam on the North Fork Toutle River is designed to help stop downstream movement of sediment near where it begins on Mount St. Helens' debris avalanche deposit.
Sediment retention dam on the North Fork Toutle River is designed to help stop downstream movement of sediment near where it begins on Mount St. Helens' debris avalanche deposit.
Angle and distance measurements to the Mount St. Helens' flanks were taken periodically to monitor for deformation similar to the 1980 bulge. Station northeast of volcano.
Angle and distance measurements to the Mount St. Helens' flanks were taken periodically to monitor for deformation similar to the 1980 bulge. Station northeast of volcano.
Fumaroles of cold, dry CO2 such as this one on a lava flow erupted in 1938 from Nyamuragira Volcano, Zaire, can be exceptionally dangerous because the gas discharge is invisible. The density difference between CO2 and air is so great that a sharp boundary can persist between them.
Fumaroles of cold, dry CO2 such as this one on a lava flow erupted in 1938 from Nyamuragira Volcano, Zaire, can be exceptionally dangerous because the gas discharge is invisible. The density difference between CO2 and air is so great that a sharp boundary can persist between them.
Large-scale poster describing USGS work.
The USGS, in cooperation with the UK Institute of Oceanographic Sciences (IOS) and others, took images of the seafloor 200 miles around the Hawaiian Islands using GLORIA. GLORIA is a long-range sonar that gives a bird’s-eye view of the seafloor.
Large-scale poster describing USGS work.
The USGS, in cooperation with the UK Institute of Oceanographic Sciences (IOS) and others, took images of the seafloor 200 miles around the Hawaiian Islands using GLORIA. GLORIA is a long-range sonar that gives a bird’s-eye view of the seafloor.