- Interior Plateau
physiographic division.
ubdivisions
It has several subdivisions, these being:
*The
Fraser Plateau
**TheChilcotin Plateau
**TheCariboo Plateau
***TheBonaparte Plateau (part of theThompson Plateau in some definitions, and also known as the Kamloops Plateau)
**TheNechako Plateau
***TheMcGregor Plateau
*TheThompson Plateau The Cariboo andChilcotin Plateau s are separate by theFraser River . TheNechako Plateau flanks the Fraser on both sides; its southern boundary is defined by theWest Road River (aka the Blackwater River) and theQuesnel River , and its northern boundary are theOmineca Mountains and theCassiar Mountains , which are two major subdivisions of theInterior Mountains .Mountain Ranges
Several mountain ranges and hill-systems are included in the definition of this region. Among these are:
*thePavilion Range includes:
**TheClear Range (includes the Scarped Range)
**TheMarble Range
**TheCornwall Hills (not formally part of the Pavilion Range, but adjoining the Clear Range on its east)
**TheTrachyte Hills (not formally part of the Pavilion Range, but adjoining the Clear and Marble Ranges on their east)
*The Arrowstone Hills (SW edge of theBonaparte Plateau )
*The Rainbow Range (sometimes assigned to either thePacific Ranges orKitimat Ranges subranges of theCoast Mountains )
*TheItcha Range
*TheIlgachuz Range
*The Quanchus Range (western edge of theNechako Plateau , in the midst of theNechako Reservoir /Ootsa Lake)
*The Telegraph Range (Nechako Plateau )
*The Fawnie Range (Nechako Plateau )
*The Pattullo Range (sometimes classified as part of theHazelton Mountains )Some classifications systems assign the Pattullo Range to the
Hazelton Mountains , which are part of the largerSkeena Mountains complex, but then theoretically also is the Quanchus Range. Also, theCariboo Mountains are sometimes included as part of the Interior Plateau.Three areas liminal to the plateau, i.e. sometimes considered part of it rather than the adjoining mountain ranges, are the
Shuswap Highland ,Okanagan Highland andQuesnel Highland .History of the Interior Plateau
The location of the
Interior Plateau inNorth America is between the Rocky Mountains and the Pacific Coast Ranges.It is cut by two rivers: the Columbia and the Fraser. The northern region is largely wooded, with the southern being
sagebrush grassland s.The first human presence was in
8500 BC .Bison remains,Clovis and other fluted points date back to this time frame. An important sites in the area is at Wenatchee site (located inWashington ).The Windust phase is dated between 10600 BC and 7100 BC. At the
Lind Coulee site in east-central Washington, leaf-shaped projectile points and knives date between 8500-5500 BC. Based on archaeological evidence, it is suggested that these people were hunters, subsisting also fromfishing and plant gathering. The presence of sea shells gives an indication that trading took place. A small oval shaped dwelling was also found at thePaulina Lake site inOregon , dating to7100 BC .The
Cascade phase took place from 7100-4300 BC, and was marked by a slight change in toolkit technology from the Windust peoples. Aresidential structure was found for this group, dating between 5500-4300 BC. Other pithouses followed between 4000-2000 BC. Most residential structures are located on rivers. During the historic era, plants andsalmon were the staple foods, which give us an indication that Cascade groups harvested salmon runs in the summer and fall.The Late Period, dated to about
2500 BC , the pithouse (quiggly hole ) came into existence. Other markers of this period include the increasing number of pithouses and settlements. Fishing continued to increase, and technology advanced, introducing more specialized barb fish spears and composite toggling harpoons. Other technology was used as well, including nets andweir s. Trade networks also flourished during this time, using sea shells, turquoise, fish grease and others.ee also
*
Columbia River Plateau
*Chilcotin Plateau Basalts References
Further reading
* Fagan, Brian M. "Ancient North America". London: Thames and Hudson, Ltd., 2005
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