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Palmer Creek is a
waterway A waterway is any navigable body of water. Broad distinctions are useful to avoid ambiguity, and disambiguation will be of varying importance depending on the nuance of the equivalent word in other languages. A first distinction is necessary b ...
in the
Kenai Peninsula The Kenai Peninsula ( Dena'ina: ''Yaghenen'') is a large peninsula jutting from the coast of Southcentral Alaska. The name Kenai (, ) is derived from the word "Kenaitze" or "Kenaitze Indian Tribe", the name of the Native Athabascan Alaskan trib ...
,
Alaska Alaska ( ; russian: Аляска, Alyaska; ale, Alax̂sxax̂; ; ems, Alas'kaaq; Yup'ik: ''Alaskaq''; tli, Anáaski) is a state located in the Western United States on the northwest extremity of North America. A semi-exclave of the U.S. ...
, US. It is an affluent of Resurrection Creek, itself a tributary of
Turnagain Arm Turnagain Arm ( Dena'ina: ''Tutl'uh'') is a waterway into the northwestern part of the Gulf of Alaska. It is one of two narrow branches at the north end of Cook Inlet, the other being Knik Arm. Turnagain is subject to climate extremes and large ti ...
.


Geography

Palmer Creek flows northwest for before reaching Resurrection Creek. Hope is located to the north. Its upper portion flows for through a broad, round-bottomed valley, while its lower part occupies a steep, narrow canyon rut through rock in some places and through gravel benches in others. Mining has been carried on chiefly in the lower of the stream and has been confined entirely to the channel gravels. The country rock includes interbedded slates and arkoses, whose cleavage strikes a little east of north and dips at a high angle. The arkoses are frequently very much jointed and in weathering do not break into small pieces as easily as do the slates, a fact readily seen on examining tho stream wash. The gravels resemble the country rock in their composition, and were undoubtedly derived from it in large part, although there are a few granitic bowlders which may not be of local origin. There is a large proportion of angular fragments and no small percentage of coarse material, possibly 5 percent being over in diameter. At the surface, the gravels were laid down without definite arrangement but are rudely stratified below. Palmer Creek gold is coarse and heavy, flattened, and smooth. In color, it is bright yellow or whitish. Pieces of native silver have been noted.


History

Gold was found on Palmer Creek in 1894 by George Palmer, a trader in the Knik Arm area in the late 1800s. These discoveries led to prospecting on neighboring streams, and in the following year (1895) the first stakes were driven on Mills Creek by S. J. Mills, whose name it bears, and at the forks of Sixmile Creek, also named by Mills. The gold claims on this stream were originally held by single individuals. Two hydraulic plants were at work in 1904, employing approximately 10 men. By 1915, the whole of the lower canyon portion, 18 claims, was controlled by one company. In 1915, it was reported that most of the prospects on Palmer Creek were on a mineralized acidic dike. The dike was first discovered in 1898 on Coeur d'Alene Gulch by an Australian outfit, but no development work was done. Later, John Hirshey and Elmer Carlson located the dike in Ptarmigan Gulch about a mile south of the original discovery and W. A. Logman relocated the dike on Coeur d'Aleno Gulch. The Lucky Strike mine, managed by John Hirshey, reported activity in 1931.


References

* {{authority control Rivers of the Kenai Peninsula Rivers of Kenai Peninsula Borough, Alaska Rivers of Alaska