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Mount St. Helens -
Summary of Volcanic History


-- Excerpt modified from: Doukas, 1990, U.S. Geological Survey Bulletin 18591 unless subscripted otherwise.
(Eruptive stages and periods are separated by dormant intervals for which no unequivocal volcanic products have been recognized. Years before 1980 are based on tree-ring dates (Yamaguchi, 1983), Carbon14 ages, and (or) historical records. A.D. dates during the Goat Rocks and Kalama eruptive periods from Yamaguchi (1983, 1985). All tephras consist of multiple layers not subdivided further here; only the thickest layers of W, B, and Y tephras are distinguished. After Crandell and others (1981), Mullineaux and Crandell (1981), and Crandell (1988))1
Eruptive stages and periods Eruptive products
Spirit
Lake
Eruptive
Stage
Modern
eruptive period
Began 1980
  • Avalanche
  • Lateral blast
  • Blast deposita
  • Lahars
  • Pyroclastic flows
  • Tephra
  • Domes (dacitic)
Goat Rocks
eruptive period
150-100 years B.P.
  • Dome (dacitic)
  • Lava flows (andesitic)
  • 19th Century Lithic Ash - 1842(?)2
A.D. 1800
  • T tephra (dacitic)
Kalama
eruptive period
500-338 years B.P.
  • Pyroclastic flows (dacitic, andesitic)
A.D. 1647?
  • Summit dome (dacitic)
  • Lahars from summit
  • Lava flows (andesitic)
  • X tephra (andesitic)
A.D. 1482
  • We tephra
A.D. 1480
  • Wn tephra
Sugar Bowl
eruptive period
1,200 years B.P.
  • Dome (dacitic) -- Northeast flank of volcano
  • Pyroclastic flows (dacitic)
  • Deposits of lateral blast (dacitic)
  • D tephra2
Castle Creek
eruptive period

(first appearance of mafic magma at the surface, which initiated the modern Mount St. Helens)2

2,500-1,600 years B.P.
  • Bu tephra (basaltic)
  • Bi tephra (dacitic)
  • Bo tephra (andesitic)
  • Bh tephra (andesitic)
  • Lava flows (basaltic)
  • Pyroclastic flows (dacitic, andesitic)
Pine Creek
eruptive period
3,000-2,500 years B.P.
  • P tephra (dacitic)
  • Pyroclastic flows (dacitic)
  • Domes (dacitic)
  • Lahars
Smith Creek
eruptive period
4,000-2,200 years B.P.
  • Ye tephra (dacitic)
  • Pyroclastic flows (dacitic)
  • Yn tephra (dacitic)
A dormant period of more than 6,000 years2
10,500 - 4,000 years ago
Swift Creek
eruptive stage
13,700-9,200 years B.P.1
(between about 13,000 and 10,500 years ago)2
  • J tephra (dacitic)
  • Pyroclastic flows (dacitic)
  • Lahars
  • Domes (dacitic)
  • S tephra (dacitic)
Mostly dormant interval of about 5,000 years2
Fraser Glaciation
ended approximately 13,000 years B.P.
Cougar
eruptive stage
20,400-19,200 years B.P.1
(began about 20,500 years ago, lasted only 2,000-3,000 years)2
  • K tephra (dacitic)
  • Pyroclastic flows (dacitic)
  • Domes (dacitic)
  • Avalanche
  • Lava flows (andesitic)
  • M tephra (dacitic)
Mostly dormant interval of about 15,000 years2
Ape Canyon
eruptive stage
approximately 40,000?-25,000 years B.P.
  • C tephra (dacitic)
  • Pyroclastic flows (dacitic)
  • Lahars
a The term "blast deposit" is here used to designate a deposit resulting from any process initiated by the lateral explosion. Precise transport and deposition mechanisms are controversial (Walker and McBroome, 1983; Hoblitt and Miller, 1984; Waitt, 1984a; Walker and Morgan, 1984)

1 -- Michael P. Doukas, 1990, Road Guide to Volcanic Deposits of Mount St. Helens and Vicinity, Washington: U.S.Geological Survey Bulletin 1859, 53p.

2 -- Donal R. Mullineaux, 1996, Pre-1980 Tephra-Fall Deposits Erupted From Mount St. Helens, Washington: USGS Professional Paper 1563.


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08/20/04, Lyn Topinka