Earth History GEOL 2110 The Paleozoic Era Cambrian and Ordovician History of Minnesota and Wisconsin Major Concepts • When sea-level rose in the Cambrian and Ordovician (Sauk and Tippecanoe Trangressions), the mid-continent of Laurentia was low lying, but with some broad topographic highs (Wisc. Dome, Transcontinental Arch, Sioux Highland, Taylors Falls Volcanic Islands) and lows (Hollandale Embayment). • Four major transgressive cycles are represented by stratigraphic sequences of sandstoneshalelimestone in Minnesota and Wisconsin. Regressions are marked by regressive sands capped by unconformities. • The purity and coarseness of the Cambrian and Ordovian quartz sandstone formations have made them important sources for glass –making and other industrial uses over the decades. However, they are currently highly sought after as sources of natural proppants for use in hydrofracing extraction of oil and gas. Geologic Timescale in Minnesota Today’s Lecture Evolution of the Penokean Mountains JAY COOKE HIBBING St. CLOUD 1,000,000,000 Years Ago Minnesota becomes the stable interior of the North American Continent 500,000,000 Years Ago Shallow seas begin to periodically flood Minnesota Laurentia Set Adrift from Rodinia Early Paleozoic Epicontinental Seas Distribution of Cambrian Sediments over Laurentia MCR Warping of the Craton • Broad horizontal tectonic stresses related to plate motion • Sediment loading • Isostatic adjustments due to different densities within the crust Paleogeography of Middle Laurentia in the Early Paleozoic Depositional Environments in Cambrian Epiric Seas From A. Runkel (MGS) Transgression of Depositional Environments Regression No Deposition/Erosion The Jordan Unconformity Transgressive - Regressive Cycles of the Hollandale Embayment The Actual Picture Storms, Trans-Regress Mini-cycles Greatly Vertically Exaggerated From A. Runkel (MGS) Ordovician Rocks of the Mississippi River Bluffs P-Platteville Limestone G-Glenwood Shale S-St. Peter Sandstone G-- P S Indian Mounds Park Minnehaha Falls P G-- S P G-S Ford Dam and Lock Fossil Hunting in the Twin Cities Lilydale Park (the Brickyards) Silica Sand Resources in SE Minnesota and SW Wisconsin Mined since the late 1800’s silica-rich sandstone current and proposed sand mines Currently 36 in WI, 7 in MN, 178 in US In 2012, 70% of US silica sand goes to 30% to Hydrofracking for Oil and Gas Use Silica Sand in Hydrofracing for Oil and Gas Drilling Ideal Proppant Characteristics • • • • • • Strong - crush resistant Med-crs sand size (16-70 mesh) Rounded and well sorted Homogeneous physical properties Low specific gravity Low cost and accessible High Purity Quartz Sandstone Formations >95% Qtz ~5mm 18 =1mm 60=.25mm 100=.15 mm OPPOSITION TO EXPANSION OF SILICA SAND MINING Concerns: - Transportation (truck traffic, road degradation, noise, safety, dust) • high road use taxes, noise and dust abatement - Air quality, silicosis? • wetting, minimal crushing - Water quality and quantity issues • recycling -Landscape alterations • reclamation plans up front - Opposition to end use-hydrofrac drilling for oil and gas Most operations are currently regulated to varying degrees by State and County level ordinances. Key questions How does SS mining differ from aggregate mining that has been practiced and regulated for decades? What is the magnitude and duration of the expansion? Next Lecture The Paleozoic Era The Silurian and Devonian Periods – Part 1 Quiz on Chapter 12 and MaG-Pz