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- W2328463421 abstract "The eruption of the prehistoric volcano, Mount Mazama, that formed the caldera holding Crater Lake in the Cascade Range of southern Oregon, occurred between 5,000 and 10,000 years ago (Williams, 1941). This volcanic activity resulted in the deposition of a pumice mantle, that extends with diminishing thickness to the east and north of Crater Lake. The depth of the pumice varies from more than 10 feet in the vicinity of Crater Lake to several inches about 100 miles to the north. The pumice lies chiefly on the east slope of the Cascade Range. This cataclysmic event and the enormous amount of pumice and other types of ?jecta deposited in this region must have had a profound effect upon the forests that existed at the time of the eruption. Forests in the immediate vicinity of Mount Mazama were probably instantly destroyed by the fragmentai ?jecta and the incandescent gases that descended the slopes of the mountain. Forests growing beyond the influence of these factors were probably less precipitately destroyed by the pumice mantle and the sudden change in the edaphic conditions. In areas still farther removed from Mount Mazama the forests were not killed, but the change in the edaphic conditions must have inhibited the growth of seedlings of those species that composed the existent forests. Eventually, as the trees of these forests died of old age or were destroyed by wind, fire, or disease, they were replaced by other species less exacting as to soil requirements. Such species were further benefited by lack of competition." @default.
- W2328463421 created "2016-06-24" @default.
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- W2328463421 date "1942-03-01" @default.
- W2328463421 modified "2023-09-25" @default.
- W2328463421 title "Post-Mount Mazama Forest Succession on the East Slope of the Central Cascades of Oregon" @default.
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- W2328463421 doi "https://doi.org/10.2307/2421018" @default.
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