The Mackenzie Basin

This mistake broadens the range of old people and may be part of a wider deformation area, Ireland Creek Fault Zone (Fox '87, Cox & Barrell '07). Over the past 5000 years, based on the age of the gravel slope along the fault trajectory, the ICF major event repetition interval was 1290 ± 90 years (McSaveney '91). In 1983, Pickle and Erwin conducted a preliminary earthquake survey of Lake Tekapo. The earthquake exceeded the bottom of the lake by about 25 meters. They classify sediments of the Godley River (Godley Glacier) and the Cass River as the main river.

People in McKenzie and the Yukon River Valley live in a vast house. As with most indigenous people in the country, the Mackenzie and the Yukon basin are mainly daily living. Thus, indigenous peoples are divided into several groups of different families. Each group is in a separate area, each group has an individual boundary defined by tradition and usage, and the team leader is selected based on the needs of the group at a particular time. For example, in reindeer hunting, the most skilled hunter is chosen as leader.

Linguistic evidence suggests that when living in the McKenzie Basin of Canada the original group formed its own tribe or related tribal groups. In this area, the ancient Apache is connected with other language groups occupying the inland of the northern Pacific coast and basin from Alaska to Oregon. This suggests that the history of the first immigration straddled the Bering Strait and was divided into several subgroups. Approximately 1500 years ago, Apache dialect broke through these related languages ​​and developed independently for the next 300 years. Approximately 700 years ago - 800 years ago, these ancient Apache began to south to the current United States. Questions about whether Apache enters the southwest on the west or east route are everywhere.