Port Snettisham

Geography

The entrance to Port Snettisham is on the northeast side of Stephens Passage, to the east of Admiralty Island, about 50 km southeast of Juneau and 30 km from the Canada–US border to the east. The eastern shore to the north of Point Windham is a very large bay which is divided into two bays. The first bay is called the Holkham Bay and the other bay is named as Port Snettisham. Snettisham is an inland water way in the system of waterways in the partially protected system along the coasts of southeastern Alaska and Canada. It is a deep water bay which was proposed to be developed to facilitate transportation of magnetite.

The fiord has three branches. At the head of North Arm is Speel River, a swift-flowing stream which enters the Coast Range for a distance of 18 mi. The tributary to East Arm, a much shorter inlet, is Whiting River, traversing the mountain system for 35 mi, though not crosscutting it. This river is navigable in small boats for about 4 mi from the mud flats at its mouth. At the head of South Arm are extensive flats which are bare at low water for a distance of 1 mi, and back of these is a low valley 5 mi in length connecting with Holkham Bay. From the shore line, the land rises abruptly to peaks reaching heights of 4000 -. The Snettisham Peninsula, a promontory with peaks averaging 2500 ft in elevation, is connected with the mainland by a low pass less than 100 ft above tide level. Snettisham post office is situated on the north end of this peninsula and 3 mi inside the entrance to Port Snettisham.

People

Historically, the Taku people have had several settlements at Port Snettisham, and still visit the area to fish, particularly for sockeye salmon.

Economy

Several mineral deposits were discovered in the drainage basin of the port. The iron ore deposits identified in 1954 were located in a stretch of about 1000 ft to southwest of the Sentinel Point extending into the southeastern shore line of the port. It was suggested in 1954 to establish a small dock, deep enough for large ocean-going vessels. Of all the deposits developed, gold was the chief mineral output, mined by the Alaska Snettisham Gold Mining Company which was established on the south shore of the Port Snettisham, 3 mi from the entrance.

The quartz ledge which constitutes the Crystal Mine was discovered by B. Heins in 1895. A 20-stamp mill was in operation by 1901. This mine was purchased in 1903 by the Alaska Snettisham Gold Mining Company, but operations were discontinued by 1905.

The Port Snettisham Iron Ore Property is located in Port Snettisham, and includes 49 contiguous properties, encompassing an area of 1012 acre, under an agreement between Arrowstar Resources Ltd. (formerly Gulfside Minerals) and Pacific Rim Mineral.

References

• This article contains public domain text from A.C. Spencer's "The Juneau gold belt, Alaska: A reconnaissance of Admiralty Island, Alaska" (1906)

References

1. [https://geonames.usgs.gov/pls/gnispublic/f?p=gnispq:3:::NO::P3_FID:1408224 USGS GNIS Feature Detail Report: Port Snettisham]
2. (1869). "Pacific coast: coast pilot of Alaska, first part, from southern boundary to Cook's Inlet". G.P.O..
3. (1906). "The Juneau gold belt, Alaska: A reconnaissance of Admiralty Island, Alaska". Government Printing Office.
4. (1946). "Haa Aani, Our Land: Tlingit and Haida Land Rights and Use". University of Washington Press.
5. "Studies of the Snettisham Magnetite Deposit, Southeastern Alaska". Bureau of Mines, United States Department of the Interior.
6. "Alaska". Arrowstar Resources.com.