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Yes, the Map Showing Lava-Flow Hazards Zones on Hawai'i Island is still accurate. It was most recently revised in 1992.
The map is intended to communicate long-term lava-flow hazards, rather than short-term hazards, which can change daily during periods of eruptive activity.
Hazard assessments are based on the assumption that future eruptions will be similar to those in the past. For the past 200 years, eruptions of Kīlauea and Mauna Loa have occurred at their summits and/or along one of their rift zones—and future eruptions on these volcanoes are likely to occur in the same areas.
Learn more: Hawaiian Volcano Observatory Frequently Asked Questions and Answers about Lava-Flow Hazards
Vog poses a health hazard by aggravating preexisting respiratory ailments. Sulfur dioxide (SO 2 ) gas can irritate skin and the tissues and mucous membranes of the eyes, nose, and throat, and can penetrate airways, producing respiratory distress in some individuals. Aerosol particles in vog can also penetrate deep into human lungs and, at elevated levels, can induce symptoms of asthma. Physical...
Lava-flow hazard zones on Hawai'i Island reflect the long-term hazard of lava flows, not the short term hazard. Rate of lava coverage—not how recently lava covered an area—is the basis of long-term lava flow hazard. Zone 1: "Includes the summits and rift zones of Kīlauea and Mauna Loa (left) where vents have been repeatedly active in historic time." These areas are the most dangerous because all...
An option is to contact the State of Hawaii Department of Commerce and Consumer Affairs . The USGS Lava-Flow Hazard Zone Map is meant to convey relative volcanic hazard rather than risk. A volcanic hazard is a destructive event that can occur in a given area or location, such as a lava flow or a volcanic earthquake, along with the probability of the event's occurrence. It is important to be aware...
The Map Showing Lava-Flow Hazard Zones on Hawai'i Island reflects long-term lava-flow hazards based on geologic data: the behavior of Hawaiian volcanoes over decades to centuries, the distribution and ages of lava flows and volcanic vents, the structure of the volcano, and topography. The map will not be revised until the geologic processes/structures/topography of the volcanoes change enough to...
The hazard zones for Hawai'i Island are based on: The locations of probable eruption sites (which are based on past eruption sites) The likely paths of lava flows erupted from those sites (based on topography and the paths of previous lava flows) The frequency of lava flow inundation of an area over the past several thousand years. The hazard zones also take into account structural and topographic...
Scientists use the term magma for molten rock that is underground and lava for molten rock that breaks through the Earth's surface.
Rising gradually to more than 4 km (2.5 mi) above sea level, Hawaii’s Mauna Loa is the largest active volcano on our planet. Its submarine flanks descend to the sea floor an additional 5 km (3 mi), and the sea floor in turn is depressed by Mauna Loa's great mass another 8 km (5 mi). This makes the volcano's summit about 17 km (10.5 mi) above its base! Learn more: USGS Hawaiian Volcano Observatory
Not usually. Earthquakes associated with eruptions rarely exceed magnitude 5, and these moderate earthquakes are not big enough to destroy buildings and roads. The largest earthquakes at Mount St. Helens in 1980 were magnitude 5, large enough to sway trees and damage buildings, but not destroy them. During the huge eruption of Mount Pinatubo in the Philippines in 1991, dozens of light to moderate...
Very hot!! Here are some temperatures recorded at different times and locations: The eruption temperature of Kīlauea lava is about 1,170 degrees Celsius (2,140 degrees Fahrenheit). The temperature of the lava in the tubes is about 1,250 degrees Celsius (2,200 degrees Fahrenheit). The tube system of episode 53 (Pu'u O'o eruption) carried lava for 10 kilometers (6 miles) from the vent to the sea...
Title: What on Earth is going on at Kilauea Volcano?
Title: What on Earth is going on at Kilauea Volcano?
After slowly moving downslope from Kīlauea Volcano’s East Rift Zone since June 27, 2014, this active lava flow in Hawaiʻi reached the town of Pāhoa just before Halloween, destroying roads, a cemetery, and private property in this community.
After slowly moving downslope from Kīlauea Volcano’s East Rift Zone since June 27, 2014, this active lava flow in Hawaiʻi reached the town of Pāhoa just before Halloween, destroying roads, a cemetery, and private property in this community.
The United States has 169 active volcanoes. More than half of them could erupt explosively, sending ash up to 20,000 or 30,000 feet where commercial air traffic flies. USGS scientists are working to improve our understanding of volcano hazards to help protect communities and reduce the risks.
Video Sections:
The United States has 169 active volcanoes. More than half of them could erupt explosively, sending ash up to 20,000 or 30,000 feet where commercial air traffic flies. USGS scientists are working to improve our understanding of volcano hazards to help protect communities and reduce the risks.
Video Sections:
--fissures...fountains...and flows
by Matthew Patrick, USGS, Hawaiian Volcano Observatory
--fissures...fountains...and flows
by Matthew Patrick, USGS, Hawaiian Volcano Observatory
In July 2010, lava erupted from Kilauea Volcano's east rift zone burned vegetation on the coastal plain as active flows advanced toward Kalapana Gardens, the same area inundated by lava flows in 1990. Two homes in the subdivision were destroyed by lava in 2010 -- one in July and one in November.
In July 2010, lava erupted from Kilauea Volcano's east rift zone burned vegetation on the coastal plain as active flows advanced toward Kalapana Gardens, the same area inundated by lava flows in 1990. Two homes in the subdivision were destroyed by lava in 2010 -- one in July and one in November.
Flows were also active in kipukas north and south of the access road today, and were pushing through thick vegetation.
Flows were also active in kipukas north and south of the access road today, and were pushing through thick vegetation.
Map showing the extent of the July 2007 eruption flow field relative to surrounding communities. Light red is the extent of the July 2007 eruption flow field. Reddish-brown is the extent of the currently-active Quarry flow as of July 8, 2010, while bright red shows the flow field expansion of the Quarry flow mapped by HVO geologists between July 8 and 14.
Map showing the extent of the July 2007 eruption flow field relative to surrounding communities. Light red is the extent of the July 2007 eruption flow field. Reddish-brown is the extent of the currently-active Quarry flow as of July 8, 2010, while bright red shows the flow field expansion of the Quarry flow mapped by HVO geologists between July 8 and 14.
A closer view of the recent flows working their way down the road and through the trees. The viewing area has been moved back once again due to its proximity to the lava flows and potential fire hazards.
A closer view of the recent flows working their way down the road and through the trees. The viewing area has been moved back once again due to its proximity to the lava flows and potential fire hazards.
View looking back to the north at the terminus of the active flow as it approaches the forested kipuka at the center of the photo. Hwy 130 is at upper right. The old ocean entry viewing area, open from 2008 to early 2010, is visible near the bottom of the photo just to the right of center.
View looking back to the north at the terminus of the active flow as it approaches the forested kipuka at the center of the photo. Hwy 130 is at upper right. The old ocean entry viewing area, open from 2008 to early 2010, is visible near the bottom of the photo just to the right of center.
Lava, on its southward journey to the ocean, crossed and buried the County lava viewing trail. The viewing area was relocated a short distance back from the flow margin.
Lava, on its southward journey to the ocean, crossed and buried the County lava viewing trail. The viewing area was relocated a short distance back from the flow margin.
A 3 meter (10 ft) high cascade feeds lava into an old quarry at the end of the Kalapana access road, within view of the County viewing area.
A 3 meter (10 ft) high cascade feeds lava into an old quarry at the end of the Kalapana access road, within view of the County viewing area.
Between the morning of September 20, 2006 and the evening of September 22, 2006, there were 10 separate breakouts from the East Lae`apuki tube about 50 meters (165 feet) inland from the older sea cliff behind the East Lae'apuki lava delta.
Between the morning of September 20, 2006 and the evening of September 22, 2006, there were 10 separate breakouts from the East Lae`apuki tube about 50 meters (165 feet) inland from the older sea cliff behind the East Lae'apuki lava delta.
Erupting vents on Mauna Loa’s northeast rift zone near Pu‘u‘ula‘ula (Red Hill) on Mar. 25, 1984, sent massive ‘a‘ā lava flows down the rift toward Kūlani.
Erupting vents on Mauna Loa’s northeast rift zone near Pu‘u‘ula‘ula (Red Hill) on Mar. 25, 1984, sent massive ‘a‘ā lava flows down the rift toward Kūlani.
Lava falls pour into 'Alae Crater at 11 p.m., HST, on August 5, 1969, supplied by a high lava fountain at Mauna Ulu, 600 m (2,000 feet) away. The falls, more than 100 m (330 ft) high and 300 m (1,000 ft) wide, had nearly filled the crater by the time the fountains stopped at 5:45 a.m., August 6.
Lava falls pour into 'Alae Crater at 11 p.m., HST, on August 5, 1969, supplied by a high lava fountain at Mauna Ulu, 600 m (2,000 feet) away. The falls, more than 100 m (330 ft) high and 300 m (1,000 ft) wide, had nearly filled the crater by the time the fountains stopped at 5:45 a.m., August 6.
Part 1 of 5
An HVO geologist photographs a small breakout covering the last stretch of exposed asphalt near the intersection of highways 130 and 137, just west of the current County lava viewing area.
An HVO geologist photographs a small breakout covering the last stretch of exposed asphalt near the intersection of highways 130 and 137, just west of the current County lava viewing area.
Vog poses a health hazard by aggravating preexisting respiratory ailments. Sulfur dioxide (SO 2 ) gas can irritate skin and the tissues and mucous membranes of the eyes, nose, and throat, and can penetrate airways, producing respiratory distress in some individuals. Aerosol particles in vog can also penetrate deep into human lungs and, at elevated levels, can induce symptoms of asthma. Physical...
Lava-flow hazard zones on Hawai'i Island reflect the long-term hazard of lava flows, not the short term hazard. Rate of lava coverage—not how recently lava covered an area—is the basis of long-term lava flow hazard. Zone 1: "Includes the summits and rift zones of Kīlauea and Mauna Loa (left) where vents have been repeatedly active in historic time." These areas are the most dangerous because all...
An option is to contact the State of Hawaii Department of Commerce and Consumer Affairs . The USGS Lava-Flow Hazard Zone Map is meant to convey relative volcanic hazard rather than risk. A volcanic hazard is a destructive event that can occur in a given area or location, such as a lava flow or a volcanic earthquake, along with the probability of the event's occurrence. It is important to be aware...
The Map Showing Lava-Flow Hazard Zones on Hawai'i Island reflects long-term lava-flow hazards based on geologic data: the behavior of Hawaiian volcanoes over decades to centuries, the distribution and ages of lava flows and volcanic vents, the structure of the volcano, and topography. The map will not be revised until the geologic processes/structures/topography of the volcanoes change enough to...
The hazard zones for Hawai'i Island are based on: The locations of probable eruption sites (which are based on past eruption sites) The likely paths of lava flows erupted from those sites (based on topography and the paths of previous lava flows) The frequency of lava flow inundation of an area over the past several thousand years. The hazard zones also take into account structural and topographic...
Scientists use the term magma for molten rock that is underground and lava for molten rock that breaks through the Earth's surface.
Rising gradually to more than 4 km (2.5 mi) above sea level, Hawaii’s Mauna Loa is the largest active volcano on our planet. Its submarine flanks descend to the sea floor an additional 5 km (3 mi), and the sea floor in turn is depressed by Mauna Loa's great mass another 8 km (5 mi). This makes the volcano's summit about 17 km (10.5 mi) above its base! Learn more: USGS Hawaiian Volcano Observatory
Not usually. Earthquakes associated with eruptions rarely exceed magnitude 5, and these moderate earthquakes are not big enough to destroy buildings and roads. The largest earthquakes at Mount St. Helens in 1980 were magnitude 5, large enough to sway trees and damage buildings, but not destroy them. During the huge eruption of Mount Pinatubo in the Philippines in 1991, dozens of light to moderate...
Very hot!! Here are some temperatures recorded at different times and locations: The eruption temperature of Kīlauea lava is about 1,170 degrees Celsius (2,140 degrees Fahrenheit). The temperature of the lava in the tubes is about 1,250 degrees Celsius (2,200 degrees Fahrenheit). The tube system of episode 53 (Pu'u O'o eruption) carried lava for 10 kilometers (6 miles) from the vent to the sea...
Title: What on Earth is going on at Kilauea Volcano?
Title: What on Earth is going on at Kilauea Volcano?
After slowly moving downslope from Kīlauea Volcano’s East Rift Zone since June 27, 2014, this active lava flow in Hawaiʻi reached the town of Pāhoa just before Halloween, destroying roads, a cemetery, and private property in this community.
After slowly moving downslope from Kīlauea Volcano’s East Rift Zone since June 27, 2014, this active lava flow in Hawaiʻi reached the town of Pāhoa just before Halloween, destroying roads, a cemetery, and private property in this community.
The United States has 169 active volcanoes. More than half of them could erupt explosively, sending ash up to 20,000 or 30,000 feet where commercial air traffic flies. USGS scientists are working to improve our understanding of volcano hazards to help protect communities and reduce the risks.
Video Sections:
The United States has 169 active volcanoes. More than half of them could erupt explosively, sending ash up to 20,000 or 30,000 feet where commercial air traffic flies. USGS scientists are working to improve our understanding of volcano hazards to help protect communities and reduce the risks.
Video Sections:
--fissures...fountains...and flows
by Matthew Patrick, USGS, Hawaiian Volcano Observatory
--fissures...fountains...and flows
by Matthew Patrick, USGS, Hawaiian Volcano Observatory
In July 2010, lava erupted from Kilauea Volcano's east rift zone burned vegetation on the coastal plain as active flows advanced toward Kalapana Gardens, the same area inundated by lava flows in 1990. Two homes in the subdivision were destroyed by lava in 2010 -- one in July and one in November.
In July 2010, lava erupted from Kilauea Volcano's east rift zone burned vegetation on the coastal plain as active flows advanced toward Kalapana Gardens, the same area inundated by lava flows in 1990. Two homes in the subdivision were destroyed by lava in 2010 -- one in July and one in November.
Flows were also active in kipukas north and south of the access road today, and were pushing through thick vegetation.
Flows were also active in kipukas north and south of the access road today, and were pushing through thick vegetation.
Map showing the extent of the July 2007 eruption flow field relative to surrounding communities. Light red is the extent of the July 2007 eruption flow field. Reddish-brown is the extent of the currently-active Quarry flow as of July 8, 2010, while bright red shows the flow field expansion of the Quarry flow mapped by HVO geologists between July 8 and 14.
Map showing the extent of the July 2007 eruption flow field relative to surrounding communities. Light red is the extent of the July 2007 eruption flow field. Reddish-brown is the extent of the currently-active Quarry flow as of July 8, 2010, while bright red shows the flow field expansion of the Quarry flow mapped by HVO geologists between July 8 and 14.
A closer view of the recent flows working their way down the road and through the trees. The viewing area has been moved back once again due to its proximity to the lava flows and potential fire hazards.
A closer view of the recent flows working their way down the road and through the trees. The viewing area has been moved back once again due to its proximity to the lava flows and potential fire hazards.
View looking back to the north at the terminus of the active flow as it approaches the forested kipuka at the center of the photo. Hwy 130 is at upper right. The old ocean entry viewing area, open from 2008 to early 2010, is visible near the bottom of the photo just to the right of center.
View looking back to the north at the terminus of the active flow as it approaches the forested kipuka at the center of the photo. Hwy 130 is at upper right. The old ocean entry viewing area, open from 2008 to early 2010, is visible near the bottom of the photo just to the right of center.
Lava, on its southward journey to the ocean, crossed and buried the County lava viewing trail. The viewing area was relocated a short distance back from the flow margin.
Lava, on its southward journey to the ocean, crossed and buried the County lava viewing trail. The viewing area was relocated a short distance back from the flow margin.
A 3 meter (10 ft) high cascade feeds lava into an old quarry at the end of the Kalapana access road, within view of the County viewing area.
A 3 meter (10 ft) high cascade feeds lava into an old quarry at the end of the Kalapana access road, within view of the County viewing area.
Between the morning of September 20, 2006 and the evening of September 22, 2006, there were 10 separate breakouts from the East Lae`apuki tube about 50 meters (165 feet) inland from the older sea cliff behind the East Lae'apuki lava delta.
Between the morning of September 20, 2006 and the evening of September 22, 2006, there were 10 separate breakouts from the East Lae`apuki tube about 50 meters (165 feet) inland from the older sea cliff behind the East Lae'apuki lava delta.
Erupting vents on Mauna Loa’s northeast rift zone near Pu‘u‘ula‘ula (Red Hill) on Mar. 25, 1984, sent massive ‘a‘ā lava flows down the rift toward Kūlani.
Erupting vents on Mauna Loa’s northeast rift zone near Pu‘u‘ula‘ula (Red Hill) on Mar. 25, 1984, sent massive ‘a‘ā lava flows down the rift toward Kūlani.
Lava falls pour into 'Alae Crater at 11 p.m., HST, on August 5, 1969, supplied by a high lava fountain at Mauna Ulu, 600 m (2,000 feet) away. The falls, more than 100 m (330 ft) high and 300 m (1,000 ft) wide, had nearly filled the crater by the time the fountains stopped at 5:45 a.m., August 6.
Lava falls pour into 'Alae Crater at 11 p.m., HST, on August 5, 1969, supplied by a high lava fountain at Mauna Ulu, 600 m (2,000 feet) away. The falls, more than 100 m (330 ft) high and 300 m (1,000 ft) wide, had nearly filled the crater by the time the fountains stopped at 5:45 a.m., August 6.
Part 1 of 5
An HVO geologist photographs a small breakout covering the last stretch of exposed asphalt near the intersection of highways 130 and 137, just west of the current County lava viewing area.
An HVO geologist photographs a small breakout covering the last stretch of exposed asphalt near the intersection of highways 130 and 137, just west of the current County lava viewing area.
