SANDSTONE LAVA CAKE EarthCache

The rocks of the North Shore of Lake Superior record the last period of volcanic activity in Minnesota. This volcanism occurred 1.1 billion years ago when North America continent began to rupture along a great rift valley, which extended from the Lake Superior region southwest to Kansas. As this rift valley opened, basaltic lavas erupted into it intermittently for about 20 million years, accumulating to a thickness of up to 20 kilometers in the Lake Superior region.

With each eruption, red-hot lavas fountained from kilometer-long fissures for up to decades at a time, flooding over large areas of a barren landscapes. Flood basalt eruptions typically followed one another in geologically rapid succession, but at times there were significant intervals (thousands to millions of years) without volcanic activity. During such intervals, streams and rivers flowing over and eroding the volcanic terrain would deposit sediments into lakes in low-lying areas. When volcanic activity resumed, these sediments could in turn be buried, heated, and compacted by lava flows and transformed into sedimentary rocks. 

An example of such a geological cycle of eruption, sedimentation, and renewed volcanism appears in the cliff face across the highway from this marker. Beneath a dark-gray basalt flow is a reddish, thinly bedded siltstone, sandstone, and shale formation. Beneath these sedimentary rocks is another lava flow, which exposed in the creek bed of Cut Face Creek just north and down the hill from this road cut. This thickness indicates a prolonged lull in volcanic activity, perhaps lasting several million years. The broken-up and mineralized character of the basalt as the left side of the cliff face resembles features observed when lavas explosively encounter standing water. This and the fine sediments beneath the lava suggest that a shallow lake may have existed in the area at the time of renewed volcanism.

To log this cache E-mail me HERE.

Source:

• Display- Geological Society of Minnesota, Minnesota Department of Transportation, and the Minnesota Geological Survey 1998.
• Geology on Display: Geology and Scenery of Minnesota’s North Shore State Parks by John C. Green. 1996. 70p
• Green, J.C., 1989, Physical volcanology of mid-Proterozoic plateau lavas: The Keweenawan North Shore Volcanic Group, Minnesota: Geological Society of America Bulletin, v.101, p.486-500.