Tintina Trench

Source: Wikipedia, the free encyclopedia.

The Tintina Trench is a large northwest-southeast valley extending through

Northern Rocky Mountain Trench in British Columbia and it has its origin from the Tintina Fault.[1]

It was named by R.G. McConnell of the Geological Survey of Canada in 1904 after an indigenous word for “chief.”

The Tintina Trench crosses the

Fort Simpson, NWT
where the combined waters turn back north for the Mackenzie's long flow to the Arctic Ocean.

Communities and features of the Trench include the following:

Geology

The location of the Tintina Trench corresponds with recessive weathering rocks which have been deformed by 450 km of right lateral faulting along the Tintina Fault.

References

External links

  1. ^ Archived 2016-03-05 at the Wayback Machine