Monthly Archives: May 2014

Monashee Mountains help define the Shuswap

                Mount Fosthall is the second highest mountain in the Shuswap

The Shuswap region is defined by its watershed, which includes the rivers and streams that all eventually empty into Shuswap Lake and the South Thompson River. However, it is the Monashee Mountains that actually direct much of this flow of water. These mountains in turn form part of the Columbia Mountain Range that also includes the Selkirks, Purcells, and the Cariboo Mountains.

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The SEAS Story – A 25 Year Retrospective

https://www.youtube.com/watch?v=fFIDczEV0vQ

A look at Shuswap geology

                                                 Bastion Mountain

The Shuswap has a fascinating geological past, as below our feet is a section of a Precambrian craton called the Shuswap terrane, which is over two billion years old. Most of the rocks found in the Shuswap are metamorphic, including primarily schists, argillite, gneiss, and phyllite, formed from either igneous or sedimentary rock by heat and pressure. Plate tectonic processes created the mountains we see today. In addition to the mountains, these plate movements and earthquakes created folds and fault lines and many of these became distinct geological features.

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The rich legacy of Dr. Mary Thomas

                                                     Dr. Mary Thomas

It is rare for a Shuswap resident to achieve provincial or national recognition for the contributions they have made to society. Famed Neskonlith elder and ethnobotanist Mary Thomas is one of these select few who will be remembered in history, as her remarkable accomplishments have been recognized widely across North America. And in 2010, some 490 hectares in the Wap Creek valley, known for both its spiritual and traditional use values, was protected as a cultural heritage feature in honour of Mary and her husband Frank Krauchi who passed away in 1997.
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