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• 1. [Article] Soil weathering processes in the Findley Lake watershed

  This is the annual report from the investigators responsible for soil characterization at the Findley Lake watershed. Soil characterization is complete for two soils and is in progress on six others. Site preparation ...

  Citation × Citation Citation Abstract Copy Title: Soil weathering processes in the Findley Lake watershed Author: U.S. International Biological Program. Coniferous Forest Biome, Singer, Michael J. (Michael John), 1945-, University of Washington, Ugolini, Fiorenzo C. This is the annual report from the investigators responsible for soil characterization at the Findley Lake watershed. Soil characterization is complete for two soils and is in progress on six others. Site preparation for years 3 and 4 is complete except for lysimeter installation. Title: Soil weathering processes in the Findley Lake watershed Author: U.S. International Biological Program. Coniferous Forest Biome, Singer, Michael J. (Michael John), 1945-, University of Washington, Ugolini, Fiorenzo C. This is the annual report from the investigators responsible for soil characterization at the Findley Lake watershed. Soil characterization is complete for two soils and is in progress on six others. Site preparation for years 3 and 4 is complete except for lysimeter installation. Close

• 2. [Article] Findley Lake watershed a terrestrial-lake interface program

  Includes supplemental reports 25-A, B & C.

  Citation × Citation Citation Abstract Copy Title: Findley Lake watershed a terrestrial-lake interface program Author: Olson, R. R., Del Moral, Roger, U.S. International Biological Program. Coniferous Forest Biome, Bockheim, James G., Tsukada, M., Welch, E. B. (Eugene B.), University of Washington, Ugolini, Fiorenzo C. Includes supplemental reports 25-A, B & C. Title: Findley Lake watershed a terrestrial-lake interface program Author: Olson, R. R., Del Moral, Roger, U.S. International Biological Program. Coniferous Forest Biome, Bockheim, James G., Tsukada, M., Welch, E. B. (Eugene B.), University of Washington, Ugolini, Fiorenzo C. Includes supplemental reports 25-A, B & C. Close

• 3. [Article] Findley Lake lysimeter leachate, precipitation inflow, outflow, and throughfall data, June 1973-January 1974

  Data on soil leachate at three sites and four depths, throughfall, precipitation, and lake inflow and outflow are presented in this report.

  Citation × Citation Citation Abstract Copy Title: Findley Lake lysimeter leachate, precipitation inflow, outflow, and throughfall data, June 1973-January 1974 Author: Minden, Ralph V., U.S. International Biological Program. Coniferous Forest Biome, University of Washington, Ugolini, Fiorenzo C. Data on soil leachate at three sites and four depths, throughfall, precipitation, and lake inflow and outflow are presented in this report. Title: Findley Lake lysimeter leachate, precipitation inflow, outflow, and throughfall data, June 1973-January 1974 Author: Minden, Ralph V., U.S. International Biological Program. Coniferous Forest Biome, University of Washington, Ugolini, Fiorenzo C. Data on soil leachate at three sites and four depths, throughfall, precipitation, and lake inflow and outflow are presented in this report. Close

• 4. [Article] Soils and parent materials of Findley Lake, Snoqualmie National Forest, Washington

  Findley Lake watershed is located in the Snoqualmie National Forest and has a surface area of 259 ha (1 Mi²). The lake is at an elevation of 1128 m (3701 ft) but the ridges attain elevations of 1450 m ...

  Citation × Citation Citation Abstract Copy Title: Soils and parent materials of Findley Lake, Snoqualmie National Forest, Washington Author: U.S. International Biological Program. Coniferous Forest Biome, Bockheim, James G., University of Washington, Ugolini, Fiorenzo C. Findley Lake watershed is located in the Snoqualmie National Forest and has a surface area of 259 ha (1 Mi²). The lake is at an elevation of 1128 m (3701 ft) but the ridges attain elevations of 1450 m (4750 ft). The Cougar Mountain Formation, consisting of lava flows, conglomerate, and volcanic sandstone, underlies the basin. The area has been glaciated and covered by a number of volcanic ash layers. Carbon 14 dating of stratified charcoal has shown that tephra are present among the ashes of Mt. St. Helens-W, Mt. St. Helens-Y, and Mazama (300, 3200, and 6700 yr B.P., respectively). An extensive fire occurred 200 years ago. Abies amabilis and Tsuga heterophylla are the most common tree species of the area. Soils were mapped into groups depending upon parent material and vegetation. The following groups were recognized. Soils of talus (16.2% of total); soils of mixed materials: (1) forested (56.2%), (2) semiforested (4.3%), (3) unforested (1.6%); residual soils of the ridges: (1) forested (17.5%), (2) unforested (4.2%). The soils Include the Haplumbrept, yorthod, and Haplaquept, andic and humic. Title: Soils and parent materials of Findley Lake, Snoqualmie National Forest, Washington Author: U.S. International Biological Program. Coniferous Forest Biome, Bockheim, James G., University of Washington, Ugolini, Fiorenzo C. Findley Lake watershed is located in the Snoqualmie National Forest and has a surface area of 259 ha (1 Mi²). The lake is at an elevation of 1128 m (3701 ft) but the ridges attain elevations of 1450 m (4750 ft). The Cougar Mountain Formation, consisting of lava flows, conglomerate, and volcanic sandstone, underlies the basin. The area has been glaciated and covered by a number of volcanic ash layers. Carbon 14 dating of stratified charcoal has shown that tephra are present among the ashes of Mt. St. Helens-W, Mt. St. Helens-Y, and Mazama (300, 3200, and 6700 yr B.P., respectively). An extensive fire occurred 200 years ago. Abies amabilis and Tsuga heterophylla are the most common tree species of the area. Soils were mapped into groups depending upon parent material and vegetation. The following groups were recognized. Soils of talus (16.2% of total); soils of mixed materials: (1) forested (56.2%), (2) semiforested (4.3%), (3) unforested (1.6%); residual soils of the ridges: (1) forested (17.5%), (2) unforested (4.2%). The soils Include the Haplumbrept, yorthod, and Haplaquept, andic and humic. Close