Adams

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  • Country
  • Volcanic Region
  • Primary Volcano Type
  • Last Known Eruption
  • 46.206°N
  • 121.49°W

  • 3742 m
    12274 ft

  • 321040
  • Latitude
  • Longitude

  • Summit
    Elevation

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Most Recent Bulletin Report: September 1997 (BGVN 22:09)


Avalanche moves 5 km down the uninhabited east flank on 20 October

A sizable rock avalanche occurred during 20 October on the E side of Mount Adams. Based on seismic signals, the avalanche began at 0031 and lasted about six minutes. There were no seismic precursors.

On 21 October, a US Geological Survey scientist inspected the avalanche deposit from a small airplane. The avalanche originated at ~3,500 m elevation on the S face of The Castle, a prominent topographic knob at the head of Battlement Ridge. The source area formed an obvious, near-vertical scar roughly triangular in shape with sides ~300 m long. The summit of The Castle remained intact. The avalanche descended the Klickitat Glacier icefall and left a thin veneer of rock debris on the steep upper part of the glacier. Below ~2,500 m elevation the deposit thickened. The avalanche traveled beyond the end of the Klickitat Glacier and continued ~2 km down the valley of Big Muddy Creek, a Klickitat River tributary. The length of the avalanche track totaled ~5 km, and the width may exceed 1 km in places. The average width is ~0.5 km. Maximum deposit thickness may exceed 20 m. The volume of the avalanche debris is probably between 1 and 5 million m3.

The avalanche deposit temporarily blocked the flow of Big Muddy Creek, resulting in the formation of a small lake on the avalanche debris. By noon on 21 October the avalanche dam had breached, and flow in Big Muddy Creek did not appear unusual. Continuing hazards exist due to the threat of additional rockfalls, damming and downstream flooding. However, these hazards exist primarily in unpopulated areas deep within the backcountry of Yakima Nation lands. No evidence suggests that hazards in populated areas far downstream have increased significantly.

This avalanche appeared unrelated to a similar-sized avalanche on the W flank of Mount Adams about seven weeks earlier (31 August). This earlier avalanche consisted of about 90% snow and ice; its source was Avalanche Glacier cirque at ~ 3,650-m elevation on the upper SW flank. Both avalanches originated where rocks evidently had been weakened by intense hydrothermal alteration. Both avalanches may have been triggered in part by wet subsurface conditions associated with late-season thawing of exceptionally heavy snowpack in conjunction with early-season storms. Neither avalanche was triggered by regional earthquake or volcanic activity.

After the 20 October avalanche, a second, smaller one swept down the same path and yielded a much smaller seismic signal that began at 0729 on 24 October. Preliminary reports suggested that the second avalanche traveled only about half the distance of the first.

Mount Adams, one of the largest volcanoes in the Cascade Range, dominates the Mount Adams volcanic field in Washington's Skamania, Yakima, Klickitat, and Lewis counties and the Yakima Indian Reservation of S-central Washington (1,250 km2). At Adams, large landslides and lahars that need not be related to eruptions probably pose the most destructive, far-reaching hazard.

Information Contacts: Cascades Volcano Observatory (CVO), U.S. Geological Survey, 5400 MacArthur Blvd., Vancouver, WA 98661, USA (URL: http://volcanoes.usgs.gov/); Geophysics Program, University of Washington, Seattle, WA 98195, USA (URL: http://vulcan.wr.usgs.gov/).

The Global Volcanism Program has no Weekly Reports available for Adams.

Index of Bulletin Reports


Reports are organized chronologically and indexed below by Month/Year (Publication Volume:Number), and include a one-line summary. Click on the index link or scroll down to read the reports.

09/1997 (BGVN 22:09) Avalanche moves 5 km down the uninhabited east flank on 20 October




Bulletin Reports

All information contained in these reports is preliminary and subject to change.


09/1997 (BGVN 22:09) Avalanche moves 5 km down the uninhabited east flank on 20 October

A sizable rock avalanche occurred during 20 October on the E side of Mount Adams. Based on seismic signals, the avalanche began at 0031 and lasted about six minutes. There were no seismic precursors.

On 21 October, a US Geological Survey scientist inspected the avalanche deposit from a small airplane. The avalanche originated at ~3,500 m elevation on the S face of The Castle, a prominent topographic knob at the head of Battlement Ridge. The source area formed an obvious, near-vertical scar roughly triangular in shape with sides ~300 m long. The summit of The Castle remained intact. The avalanche descended the Klickitat Glacier icefall and left a thin veneer of rock debris on the steep upper part of the glacier. Below ~2,500 m elevation the deposit thickened. The avalanche traveled beyond the end of the Klickitat Glacier and continued ~2 km down the valley of Big Muddy Creek, a Klickitat River tributary. The length of the avalanche track totaled ~5 km, and the width may exceed 1 km in places. The average width is ~0.5 km. Maximum deposit thickness may exceed 20 m. The volume of the avalanche debris is probably between 1 and 5 million m3.

The avalanche deposit temporarily blocked the flow of Big Muddy Creek, resulting in the formation of a small lake on the avalanche debris. By noon on 21 October the avalanche dam had breached, and flow in Big Muddy Creek did not appear unusual. Continuing hazards exist due to the threat of additional rockfalls, damming and downstream flooding. However, these hazards exist primarily in unpopulated areas deep within the backcountry of Yakima Nation lands. No evidence suggests that hazards in populated areas far downstream have increased significantly.

This avalanche appeared unrelated to a similar-sized avalanche on the W flank of Mount Adams about seven weeks earlier (31 August). This earlier avalanche consisted of about 90% snow and ice; its source was Avalanche Glacier cirque at ~ 3,650-m elevation on the upper SW flank. Both avalanches originated where rocks evidently had been weakened by intense hydrothermal alteration. Both avalanches may have been triggered in part by wet subsurface conditions associated with late-season thawing of exceptionally heavy snowpack in conjunction with early-season storms. Neither avalanche was triggered by regional earthquake or volcanic activity.

After the 20 October avalanche, a second, smaller one swept down the same path and yielded a much smaller seismic signal that began at 0729 on 24 October. Preliminary reports suggested that the second avalanche traveled only about half the distance of the first.

Mount Adams, one of the largest volcanoes in the Cascade Range, dominates the Mount Adams volcanic field in Washington's Skamania, Yakima, Klickitat, and Lewis counties and the Yakima Indian Reservation of S-central Washington (1,250 km2). At Adams, large landslides and lahars that need not be related to eruptions probably pose the most destructive, far-reaching hazard.

Information Contacts: Cascades Volcano Observatory (CVO), U.S. Geological Survey, 5400 MacArthur Blvd., Vancouver, WA 98661, USA (URL: http://volcanoes.usgs.gov/); Geophysics Program, University of Washington, Seattle, WA 98195, USA (URL: http://vulcan.wr.usgs.gov/).
Download or Cite this Report

Although lower in height than its neighbor to the north, Mount Rainier, massive Mount Adams rises above a lower topographic base and is second in volume only to Mount Shasta among volcanoes of the Cascade Range. The Mount Adams volcanic field includes the 200 cu km Mount Adams complex andesitic-dacitic stratovolcano, elongated along a NNW-SSE line, and more than 60 flank vents. Volcanism began about 940 thousand years ago (ka), with three main cone-building stages occurring at about 500, 450 and 30 ka. Adams was active throughout the Holocene, producing two dozen minor explosive eruptions from summit and flank vents. Six Holocene lava flows are located on the flanks between 2100 and 2600 m altitude. The most voluminous Holocene lava flows, some of which traveled 10 km or more, were emplaced between about 7 and 4 ka. The latest eruption about 1000 years ago produced a minor tephra layer and possibly a small lava flow down the east flank.

Summary of Holocene eruption dates and Volcanic Explosivity Indices (VEI).

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
0950 (?) Unknown Confirmed 2 Tephrochronology East flank?, Tephra layer 24
0200 (?) Unknown Confirmed 2 Tephrochronology Tephra layer 23
0300 BCE (?) Unknown Confirmed 2 Tephrochronology Tephra layer 22
0400 BCE (?) Unknown Confirmed 2 Tephrochronology Tephra layer 21
0550 BCE ± 1000 years Unknown Confirmed 2 Tephrochronology Tephra layers 19-20
1850 BCE (after) Unknown Confirmed 1 Tephrochronology SSE flank (2100 m)
2650 BCE ± 300 years Unknown Confirmed 2 Tephrochronology Tephra layers 17-18
2950 BCE ± 100 years Unknown Confirmed 1 Tephrochronology SSE flank (2600 m), Tephra layer 16
3250 BCE ± 300 years Unknown Confirmed 2 Tephrochronology Tephra layer 15
3550 BCE (?) Unknown Confirmed 2 Tephrochronology Tephra layer 14
3800 BCE ± 1950 years Unknown Confirmed 1 Tephrochronology NNE flank (2100-2250 m)
4050 BCE ± 500 years Unknown Confirmed 2 Tephrochronology Upper SW flank?, Tephra layers 11-13
4550 BCE (?) Unknown Confirmed 2 Tephrochronology NW flank (2200-2400 m), Tephra layer 10
5150 BCE ± 500 years Unknown Confirmed 2 Tephrochronology Tephra layers 5-9
7050 BCE ± 1000 years Unknown Confirmed 2 Tephrochronology Tephra layers 1-4

This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.


Synonyms

Pahto | Paddo

Cones

Feature Name Feature Type Elevation Latitude Longitude
Bunnell Butte Pyroclastic cone 46° 5' 0" N 121° 27' 0" W
Goat Butte Pyroclastic cone 2281 m 46° 13' 0" N 121° 26' 0" W
Little Mount Adams Pyroclastic cone 2079 m 46° 11' 0" N 121° 25' 0" W
Potato Hill Pyroclastic cone 46° 20' 0" N 121° 30' 0" W
Red Butte Pyroclastic cone 2196 m 46° 15' 0" N 121° 28' 0" W
Smith Butte Pyroclastic cone 46° 4' 0" N 121° 28' 0" W
Snipes Mountain Pyroclastic cone 46° 6' 0" N 121° 28' 0" W
South Butte Pyroclastic cone 2316 m 46° 11' 0" N 121° 29' 0" W

Craters

Feature Name Feature Type Elevation Latitude Longitude
King Mountain Fissure Fissure vent
Mount Adams rises above a cloud layer filling valleys in the Cascade Range, viewed from High Knob, NW of the volcano. Adams is constructed on a lower base than its neighbor Mount Rainier, and has a larger volume. Unlike Mount Rainier, where eruptions have mostly been restricted to the summit conduit, Mount Adams has also produced eruptions from numerous flank vents surrounding the volcano. A series of lava flows were erupted on the north, NW, south and east flanks between about 7000 and 1000 years ago.

Photo by Lee Siebert, 1981 (Smithsonian Institution).
The elongated form of Mount Adams, constructed by eruptions along a NNW-SSE line, is seen in this view from Mount St. Helens to the west. Eruptive activity continued into the Holocene from both summit and flank vents. Vents on the north, NW, south and east flanks between 2100-2600 m altitude produced lava flows between about 7000 and 1000 years ago.

Photo by Lee Siebert, 1979 (Smithsonian Institution).
Mount Adams, the highest peak between Mount Rainier and Mount Shasta, forms a prominent backdrop to the farmlands on the east side of the Cascades. Mount Adams, known to the Columbia River Indians as Pahto or Paddo, was featured prominently in Indian legends. The summit of Adams was said to have been flattened by a mightly blow from its southern brother, Mount Hood (Wyeast), when the damsel St. Helens (La-wa-la-clough) preferred Adams over Hood.

Photo by Lee Siebert, 1982 (Smithsonian Institution).
The farmlands of the Trout Lake valley SW of Mount Adams are underlain by a massive mudflow produced by collapse of the upper SW flank of Adams about 6000 years ago. Farmers were forced to remove numerous boulders of altered rocks from near the summit of the volcano that littered the surface of the deposit, which covered 15 sq km of the Trout Lake lowland and reached as far as 60 km to the south. The source of the mudflow was a debris avalanche from the upper White Salmon glacier area, just left of the shadow beneath the summit.

Photo by Lee Siebert, 1995 (Smithsonian Institution).
Adams Glacier descends from the summit of Mount Adams, seen rising to 3742 m above Takhlakh Lake on the NW side. The main cone of Mount Adams was constructed primarily of lava flows during the Pleistocene, but flank vents produced lava flows and explosive eruptions during the Holocene. The Tahk Tahk Meadow lava flow, the largest from Mount Adams during the Holocene, originated from a vent low on the NW flank and traveled a total of 10 km, reaching several km beyond the east (left) side of Takhlakh Lake.

Photo by Lee Siebert, 1981 (Smithsonian Institution).
Mount Adams, the second highest peak in the Pacific Northwest, rises above forests in the southern Cascade Range of Washington in this view from the SW. The large cirque below the left side of the summit is occupied by the White Salmon and Avalanche Glaciers and was the source of a large mudflow that traveled 60 km down the White Salmon River valley about 6000 years ago.

Photo by Lee Siebert, 1995 (Smithsonian Institution).
The massive 4392-m-high glacier-mantled cone of Mount Rainier forms the highest peak of the Cascade Range. This aerial view from the NW also shows neighboring Mount Adams on the right horizon. The steep cirque forming the sheer Willis Wall, named after the 19th-century geologist Bailey Willis, lies in the shadow at the left, below the Winthrop Glacier, which forms the left-hand ridge of Mount Rainier. Two young overlapping cinder cones, their rims kept free of snow by high heat flow, form the flat summit of the volcano.

Photo by Lee Siebert, 1985 (Smithsonian Institution)

The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title.

Hammond P E, Pedersen S A, Hopkins K D, Aiken D, Harle D S, Danes Z F, Konicek D L, Stricklin C R, 1976. Geology and gravimetry of the Quaternary basaltic volcanic field, southern Cascade Range, Washington. In: {Proc 2nd United Nations Symp Devel Use Geotherm Resour, San Francisco}, Washington D C: U S Government Printing Office, 1: 397-405.

Harris S L, 1988. Fire Mountains of the West: the Cascade and Mono Lake Volcanoes. Missoula, MT: Mountain Press, 379 p.

Hildreth W, Fierstein J, 1997. Recent eruptions of Mount Adams, Washington Cascades, USA. Bull Volc, 58: 472-490.

Hildreth W, Lanphere M A, 1994. Potassium-argon geochronology of a basalt-andesite-dacite arc system: the Mount Adams volcanic field, Cascade Range of southern Washington. Geol Soc Amer Bull, 106: 1413-1429.

Hopkins K D, 1976. Geology of the south and east slopes of Mount Adams volcano, Cascade Range, Washington. Unpublished PhD thesis, Univ Washington, 143 p.

IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..

Katsui Y (ed), 1971. List of the World Active Volcanoes. Volc Soc Japan draft ms, (limited circulation), 160 p.

Wood C A, Kienle J (eds), 1990. Volcanoes of North America. Cambridge, England: Cambridge Univ Press, 354 p.

Volcano Types

Stratovolcano
Pyroclastic cone(s)

Tectonic Setting

Subduction zone
Continental crust (> 25 km)

Rock Types

Major
Andesite / Basaltic Andesite
Basalt / Picro-Basalt
Minor
Dacite

Population

Within 5 km
Within 10 km
Within 30 km
Within 100 km
0
70
4,019
393,303

Affiliated Databases

Large Eruptions of Adams Information about large Quaternary eruptions (VEI >= 4) is cataloged in the Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
WOVOdat WOVOdat is a database of volcanic unrest; instrumentally and visually recorded changes in seismicity, ground deformation, gas emission, and other parameters from their normal baselines. It is sponsored by the World Organization of Volcano Observatories (WOVO) and presently hosted at the Earth Observatory of Singapore.
EarthChem EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility Integrated Earth Data Applications (IEDA). IEDA is a collaborative effort of EarthChem and the Marine Geoscience Data System (MGDS).
Smithsonian Collections Search the Smithsonian's NMNH Department of Mineral Sciences collections database. Go to the "Search Rocks and Ores" tab and use the Volcano Name drop-down to find samples.