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Station: 98-PL-01

Station ID: 98-PL-01 [1] [2]
Volcano:
Collector: de Fontaine, C. S.
Date visited:
NAD83 latitude: 60.61805556
NAD83 longitude: -150.7508333
Default location: No
Location description: Paradox Lake, Kenai Peninsula, Alaska. Paradox Lake is a small (0.11 km square) meromictic lake with a high catchment-to-lake-area ratio (27) and a nearly closed surface-hydrologic system. It is located in the Kenai Lowland, within 40 km of Tustumena Lake. The oblong-shaped lake contains a single basin on the northeast end of the lake, with a maximum depth of about 16 m. Dense vegetation and steep (typically 10-18 degrees) slopes surround the lake, rising about 6 m on the northwest and southeast sides. Nearly 9-m-long cores were retrieved in 16 m water depth at the deepest part of the lake basin; Livingston corer used. Cores contain 109 tephra layers over 13,200-yr record. Coordinates provided as degrees/minutes/seconds and converted to decimal degrees; datum not specified, assumed to be NAD83.
Station Location:
Samples:
98-PL-01_<5.0
98-PL-01_17.2
98-PL-01_21.2
98-PL-01_22.2
98-PL-01_26.4
98-PL-01_30.2
98-PL-01_30.8
98-PL-01_32.6
98-PL-01_33.2
98-PL-01_43.4
98-PL-01_46.2
98-PL-01_66.2
98-PL-01_142.8
98-PL-01_149.0
98-PL-01_153.2
98-PL-01_155.2
98-PL-01_177.2
98-PL-01_184.6
98-PL-01_217.4
98-PL-01_225.4
98-PL-01_228.8
98-PL-01_229.4
98-PL-01_229.8
98-PL-01_230.8
98-PL-01_304.0
98-PL-01_316.6
98-PL-01_321.6
98-PL-01_322.6
98-PL-01_335.0
98-PL-01_351.4
98-PL-01_353.2
98-PL-01_358.0
98-PL-01_358.6
98-PL-01_379.0
98-PL-01_392.0
98-PL-01_403.4
98-PL-01_413.8
98-PL-01_416.0
98-PL-01_418.8
98-PL-01_420.6
98-PL-01_422.4
98-PL-01_454.8
98-PL-01_464.6
98-PL-01_466.0
98-PL-01_468.4
98-PL-01_470.0
98-PL-01_487.0
98-PL-01_498.4
98-PL-01_503.4
98-PL-01_505.8
98-PL-01_507.2
98-PL-01_510.4
98-PL-01_512.8
98-PL-01_514.6
98-PL-01_519.8
98-PL-01_524.0
98-PL-01_526.6
98-PL-01_539.8
98-PL-01_542.8
98-PL-01_556.2
98-PL-01_558.4
98-PL-01_562.4
98-PL-01_563.2
98-PL-01_564.2
98-PL-01_565.6
98-PL-01_566.6
98-PL-01_567.2
98-PL-01_568.6
98-PL-01_569.2
98-PL-01_573.6
98-PL-01_575.6
98-PL-01_586.8
98-PL-01_590.6
98-PL-01_591.2
98-PL-01_592.2
98-PL-01_593.2
98-PL-01_603.0
98-PL-01_606.8
98-PL-01_608.4
98-PL-01_612.6
98-PL-01_615.2
98-PL-01_616.8
98-PL-01_617.6
98-PL-01_621.4
98-PL-01_622.0
98-PL-01_636.0
98-PL-01_636.4
98-PL-01_637.4
98-PL-01_638.0
98-PL-01_640.2
98-PL-01_641.6
98-PL-01_645.0
98-PL-01_646.6
98-PL-01_738.4
98-PL-01_746.4
98-PL-01_768.2
98-PL-01_786.2
98-PL-01_792.2
98-PL-01_794.4
98-PL-01_797.8
98-PL-01_807.8
98-PL-01_814.4
98-PL-01_821.8
98-PL-01_829.0
98-PL-01_834.4
98-PL-01_838.0
98-PL-01_853.8
98-PL-01_856.0
98-PL-01_865.0
98-PL-01_874.4

References Cited

[1] Late Quaternary distal tephra-fall deposits in lacustrine sediments, Kenai Peninsula, Alaska, 2007

de Fontaine, C.S., Kaufman, D.S., Anderson, R.S., Werner, Al, Waythomas, C.F., and Brown, T.A., 2007, Late Quaternary distal tephra-fall deposits in lacustrine sediments, Kenai Peninsula, Alaska: Quaternary Research, v. 68, p. 64-78, doi:10.1016/j.yqres.2007.03.006.

[2] Late quaternary distal tephra in lacustrine sediments of the upper Cook Inlet, Alaska, 2003

de Fontaine, C. S., 2003, Late quaternary distal tephra in lacustrine sediments of the upper Cook Inlet, Alaska: Northern Arizona University unpublished M.S. thesis, 111 p.