Forum Discussion
fanrgs
Apr 22, 2015Explorer
Not sure how this thread got off topic, but the geology of the Franklin Mountains is actually fairly complicated, as can seen by reading US Geological Survey Bulletin 1298 entitled "Geology of the Northern Franklin Mountains, Texas and New Mexico." The lower portion of this range includes 5,000 feet of Precambrian metamorphic rocks cut by 1.1 billion year-old granitic rocks.
So, although not sure exactly what is meant by "continental plate rocks," this thick sequence of Precambrian rocks would certainly qualify as "basement rocks." And the Northern and Canadian Rockies consist of thousands of feet of sedimentary rocks of similar ages to those in the Franklins. In fact, it is views of those stratified sedimentary mountains that draw tourists and photographers to Glacier National Park in Montana and Banff and Jasper National Parks in Alberta.
So, although not sure exactly what is meant by "continental plate rocks," this thick sequence of Precambrian rocks would certainly qualify as "basement rocks." And the Northern and Canadian Rockies consist of thousands of feet of sedimentary rocks of similar ages to those in the Franklins. In fact, it is views of those stratified sedimentary mountains that draw tourists and photographers to Glacier National Park in Montana and Banff and Jasper National Parks in Alberta.
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