Tribal Members!  Please remember to contact the UTV office if you have moved - we need your current address and phone number!  You can contact the office by email:  utvadmin@ugashikvillage.com or call the office at: 907-338-7610

If you would like to join our tribe we do have requirements when determining eligibility status of members such as you don’t belong to another native affiliation, you can show proof of a C.I.B. and last we need a have a copy of your birth certificate. Once you qualify you may be eligible for programs Ugashik offers to members, please don’t hesitate in contacting our office.

Alaska Regional Office Bureau of Indian Affairs 3601 C Street Suite 1100 Anchorage, AK 99503-5947 Telephone: 907-271-1734 Toll Free: 1-800-645-8465 Fax: 907-271-1349

Juneau Office Bureau of Indian Affairs PO Box 21647 709 West 9th Street Juneau, AK 99802 Telephone: 907-586-7177 Toll Free: 1-800-645-8397 Telefax: 907-586-7252

Enrollment Committee

• Cheri Pingree
• Hattie Albecker
• Daniel Pingree, Sr.

Yup'ik Eskimos and Aleuts jointly occupied the area historically. This Aleut village was first recorded in 1880 as "Oogashik." In the 1890s, the Red Salmon Company developed a cannery, and Ugashik became one of the largest villages in the region. The 1919 flu epidemic decimated the population. The cannery has continued to operate under various owners. The Briggs Way Cannery opened in 1963. The village has a small year-round population.

The Ugashik-Peulik volcanic complex lies south of Becharof Lake and east of Upper Ugashik Lake. Late-Pleistocene caldera formation at Ugashik volcano was followed by the emplacement of at least 5 Holocene lava domes within the 4.5-km-wide caldera. Most of the caldera walls consist of basement sandstones of Jurassic age. Following caldera formation the small, 3 cu km Peulik stratovolcano grew 2.5 km to the north to a height of 1474 m, more than 500 m above that of Ugashik. Lava flows from Peulik cover the caldera rim to the south and extend to Becharof Lake, 6 km to the north. A small lava dome at 1200 m elevation on the east flank of Peulik was the source of a small block-and-ash flow. The summit of Peulik volcano contains a 1.5-km-wide crater breached to the west that is partially filled by a lava dome. Debris-avalanche deposits cover a 75 sq km area to the NW. A single documented historical eruption took place from Peulik volcano in 1814.