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Explosive eruption column from Halema‘uma‘u Crater 11:15 a.m. May 1...
Explosive eruption column from Halema‘uma‘u 11:15 a.m. May 18, 1924...
Explosive eruption column from Halema‘uma‘u 11:15 a.m. May 18, 1924...
Explosive eruption column from Halema‘uma‘u 11:15 a.m. May 18, 1924...

The series of explosive eruptions in May 1924 followed the withdrawal of lava from lava lake in Halema‘uma‘u Crater that began in February and the ensuing collapse of its crater floor in late April. Scientists infer that the lava had drained to a depth below the water table at the summit, currently about 500 m (1,640 ft) below the floor of the caldera.

The series of explosive eruptions in May 1924 followed the withdrawal of lava from lava lake in Halema‘uma‘u Crater that began in February and the ensuing collapse of its crater floor in late April. Scientists infer that the lava had drained to a depth below the water table at the summit, currently about 500 m (1,640 ft) below the floor of the caldera.

Park superintendent Thomas Boles after a narrow escape at Kīlauea V...
Park superintendent Thomas Boles after a narrow escape at Kīlauea, ...
Park superintendent Thomas Boles after a narrow escape at Kīlauea, ...
Park superintendent Thomas Boles after a narrow escape at Kīlauea, ...

Boles poses on the grounds of the Volcano House hotel with the Halemaumau eruption plume in the background. He fell cutting his hands and a knee while fleeing an explosion the day before. After his close call the superintendent barred all public access within two miles of Halemaumau.

Boles poses on the grounds of the Volcano House hotel with the Halemaumau eruption plume in the background. He fell cutting his hands and a knee while fleeing an explosion the day before. After his close call the superintendent barred all public access within two miles of Halemaumau.

Explosion at Halemaumau as seen from Uēkahuna Bluff, at Kīlauea Vol...
Explosion at Halema‘uma‘u as seen from Uēkahuna Bluff, at Kīlauea, ...
Explosion at Halema‘uma‘u as seen from Uēkahuna Bluff, at Kīlauea, ...
Explosion at Halema‘uma‘u as seen from Uēkahuna Bluff, at Kīlauea, ...

Eight persons, including newspaper and movie men observing the scene at Halema‘uma‘u, were caught in a rain of hot rocks from this explosion. The rocks emitted hissing sounds as hot gas, mainly steam, escaped from them. Park superintendent Thomas Boles was knocked down twice by this bombardment.

Eight persons, including newspaper and movie men observing the scene at Halema‘uma‘u, were caught in a rain of hot rocks from this explosion. The rocks emitted hissing sounds as hot gas, mainly steam, escaped from them. Park superintendent Thomas Boles was knocked down twice by this bombardment.

Observer examines boulder ejected from Halemaumau, at Kīlauea Volca...
Boulder ejected from Halemaumau, at Kīlauea, May 11, 1925
Boulder ejected from Halemaumau, at Kīlauea, May 11, 1925
Boulder ejected from Halemaumau, at Kīlauea, May 11, 1925

On May 11, Ruy Finch and W.O. Clark visited Halemaumau and found a rock fragment weighing about 180 kg (400 pounds) that had been thrown 60 meters (200 feet) from the rim of the crater.

One of the first explosion clouds from Halemaumau, at Kīlauea Volca...
First explosion clouds from Halemaumau, Kīlauea 1925
First explosion clouds from Halemaumau, Kīlauea 1925
First explosion clouds from Halemaumau, Kīlauea 1925

Later scientists at the Observatory listed May 10 as the first day of the eruptive series. Between this date and May 27, they carefully recorded all explosions, ballistic falls, electric storms, and muddy rains as well as earthquakes felt and recorded on seismographs.

Later scientists at the Observatory listed May 10 as the first day of the eruptive series. Between this date and May 27, they carefully recorded all explosions, ballistic falls, electric storms, and muddy rains as well as earthquakes felt and recorded on seismographs.

Dust cloud caused by the collapse of the Halemaumau crater floor at...
Dust cloud caused by the collapse of the Halemaumau crater floor at...
Dust cloud caused by the collapse of the Halemaumau crater floor at...
Dust cloud caused by the collapse of the Halemaumau crater floor at...

After the severe earthquake swarm in lower Puna subsided, seismic tremor became more pronounced at the summit of Kīlauea Volcano. The floor of the crater of Halemaumau continued to collapse.

Scientists looking into the bright glow of Mauna Loa's 1942 eruptiv...
Scientists looking into bright glow of Mauna Loa's 1942 eruptive ve...
Scientists looking into bright glow of Mauna Loa's 1942 eruptive ve...
Scientists looking into bright glow of Mauna Loa's 1942 eruptive ve...

Scientists looking into the bright glow of Mauna Loa's 1942 eruptive vent. Eruption occurred during WWII and was not publicized to prevent Japanese war planes from navigating to the island at night.

Earthquake damage on road at Kapoho, Hawai‘i. ...
Earthquake damage on road at Kapoho, Hawai‘i.
Earthquake damage on road at Kapoho, Hawai‘i.
Earthquake damage on road at Kapoho, Hawai‘i.

On April 22, an observer at the Kapoho railroad quarry counted 238 felt earthquakes over a period of four hours. By Sunday, April 27, things had calmed considerably at Kapoho, although a dozen shocks were felt during the day and half a dozen more overnight.

On April 22, an observer at the Kapoho railroad quarry counted 238 felt earthquakes over a period of four hours. By Sunday, April 27, things had calmed considerably at Kapoho, although a dozen shocks were felt during the day and half a dozen more overnight.

Railroad tracks buckled at fault boundary at Kapoho, Hawai‘i...
Railroad tracks buckled at fault boundary at Kapoho, Hawai‘i
Railroad tracks buckled at fault boundary at Kapoho, Hawai‘i
Railroad tracks buckled at fault boundary at Kapoho, Hawai‘i

These tracks were damaged by the vertical drop along the zone of cracks and faults that ran parallel to the east rift zone of Kīlauea Volcano. Witnesses reported that where the railroad entered the valley, the ties and rails were swinging like a suspension bridge for a distance of about 61 meters (200 feet).

These tracks were damaged by the vertical drop along the zone of cracks and faults that ran parallel to the east rift zone of Kīlauea Volcano. Witnesses reported that where the railroad entered the valley, the ties and rails were swinging like a suspension bridge for a distance of about 61 meters (200 feet).

Kapoho, Hawai‘i residents in lower Puna await evacuation during sei...
Kapoho, Hawai‘i residents in lower Puna await evacuation during sei...
Kapoho, Hawai‘i residents in lower Puna await evacuation during sei...
Kapoho, Hawai‘i residents in lower Puna await evacuation during sei...

By April 22, 1924, the incessant earthquakes caused many people to leave the district. When Hilo Tribune Herald reporter Jazz Belknap reached the Kapoho train station, he found a great crowd waiting for the autos that were hauling passengers out of the district.

By April 22, 1924, the incessant earthquakes caused many people to leave the district. When Hilo Tribune Herald reporter Jazz Belknap reached the Kapoho train station, he found a great crowd waiting for the autos that were hauling passengers out of the district.

Photograph of many steaming fumaroles on a broad plain surrounded by mountains
Valley of Ten Thousand Smokes, Katmai, Alaska, circa 1922
Valley of Ten Thousand Smokes, Katmai, Alaska, circa 1922
Valley of Ten Thousand Smokes, Katmai, Alaska, circa 1922

Valley of Ten Thousand Smokes in Katmai National Park, circa 1922. Windy Creek is in the foreground. Following the June 6, 1912 eruption of Novarupta-Katmai, thousands of fumaroles filled the valley for many years. Buried snow fields, glacial streams, and precipitation were converted to steam by the heat trapped in the pyroclastic flow.

Valley of Ten Thousand Smokes in Katmai National Park, circa 1922. Windy Creek is in the foreground. Following the June 6, 1912 eruption of Novarupta-Katmai, thousands of fumaroles filled the valley for many years. Buried snow fields, glacial streams, and precipitation were converted to steam by the heat trapped in the pyroclastic flow.

black and white photo showing a 3-story home tilted to the right
1906 Earthquake Damage to Home in San Francisco
1906 Earthquake Damage to Home in San Francisco
1906 Earthquake Damage to Home in San Francisco

1906 earthquake damage to home on Howard and 17th Streets in San Francisco. Liquefaction, the phenomenon of saturated soils losing their stiffness and strength during shaking, caused structures to tilt and collapse.

1906 earthquake damage to home on Howard and 17th Streets in San Francisco. Liquefaction, the phenomenon of saturated soils losing their stiffness and strength during shaking, caused structures to tilt and collapse.

View from the sky of a city and its waterfront with various ships docked, and most buildings on land are ruined.
San Francisco in ruins, 1906
San Francisco in ruins, 1906
San Francisco in ruins, 1906

One of the most well-known photographs by George R. Lawrence, taken May 28, 1906, about 6 weeks after the Great San Francisco earthquake which occurred on April 18. The 160-degree panorama was taken from a camera suspended from a kite 2,000 feet in the air. The view looks up Market Street with the waterfront and Union Ferry Building in the foreground.

One of the most well-known photographs by George R. Lawrence, taken May 28, 1906, about 6 weeks after the Great San Francisco earthquake which occurred on April 18. The 160-degree panorama was taken from a camera suspended from a kite 2,000 feet in the air. The view looks up Market Street with the waterfront and Union Ferry Building in the foreground.

Boulder Creek leading from Mount Baker, Washington is a hydrology m...
Boulder Creek leading from Mount Baker, WA is a hydrology monitorin...
Boulder Creek leading from Mount Baker, WA is a hydrology monitorin...
Boulder Creek leading from Mount Baker, WA is a hydrology monitorin...

Boulder Creek leading from Mount Baker, Washington is a hydrology monitoring site where water is collected and measured for chemicals that may signal volcanic unrest.

Lahar deposit cross section in the Trout Lake lowland, which origin...
Lahar deposit cross section in the Trout Lake lowland, which origin...
Lahar deposit cross section in the Trout Lake lowland, which origin...
Lahar deposit cross section in the Trout Lake lowland, which origin...

Lahar deposit cross section in the Trout Lake lowland, which originated from Mount Adams. Thickness of deposit is about 2.5 m (8 ft).

North Sister's steep northeast face, thick summit lava flow makes u...
North Sister's steep NE face, thick summit lava flow makes up "Glis...
North Sister's steep NE face, thick summit lava flow makes up "Glis...
North Sister's steep NE face, thick summit lava flow makes up "Glis...

Remnant of Villard Glacier is in cirque below. Thick summit lava flow makes up "Glisan Pinnacle," which overlies hundreds of thin rubbly lava flows that are intercalated with red-oxidized agglutinate and scoria falls exposed on 800-m- (2600-ft-) high face below. Flows that form ridge at upper right are thicker than those on most of edifice.

Remnant of Villard Glacier is in cirque below. Thick summit lava flow makes up "Glisan Pinnacle," which overlies hundreds of thin rubbly lava flows that are intercalated with red-oxidized agglutinate and scoria falls exposed on 800-m- (2600-ft-) high face below. Flows that form ridge at upper right are thicker than those on most of edifice.

Sherman Crater, Mount Baker, Washington. Postcard photograph taken ...
Sherman Crater, Mount Baker, WA. Postcard photograph taken from sou...
Sherman Crater, Mount Baker, WA. Postcard photograph taken from sou...
Baker Lake shorelines were closed during 1975 increase in Mount Bak...
Baker Lake shorelines were closed during 1975 increase in Mount Bak...
Baker Lake shorelines were closed during 1975 increase in Mount Bak...
Baker Lake shorelines were closed during 1975 increase in Mount Bak...

This notice was posted at campgrounds around Baker Lake by the US Forest Service in June 1975. Normally, Baker Reservoir approaches capacity during mid-summer. At most other times, reservoir levels are low enough to impound lahars the size of those that occurred in 1843.

This notice was posted at campgrounds around Baker Lake by the US Forest Service in June 1975. Normally, Baker Reservoir approaches capacity during mid-summer. At most other times, reservoir levels are low enough to impound lahars the size of those that occurred in 1843.

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