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(Geology of Ice Age National Scientific Reserve of Wisconsin)Create a 12- to 15 slide MicrosoftPowerPoint® presentation for your chosen geologic feature.
Address the following: Describe the various geologic events that have occurred in the region around your feature. Describe the geological features and various types of rocks that formed in the area, such as mountains, craters, canyons, volcanoes, fault lines, or folds. What is the most prevalent rock type of your feature? Describe the rock type’s mineral composition. How old is your geologic feature? Estimate the absolute age of the feature, and discuss methods used to determine the age. What geologic event created your feature? Discuss the process of plate tectonics related to the formation. Explain the significance of igneous, sedimentary, and metamorphic rocks in your region. Describe the types of weathering and erosion processes that have likely affected the physical appearance of your feature. Describe any significant water, ocean, desert, or glacial features associated with your region, and the process involved with creating one of them. Explain what resources are abundant in the region and the importance and economic value of these resources to the region. In conclusion, explain why you selected this geologic feature for your presentation. Include graphics. Include details in speaker notes
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First Slide
Changes in weather patterns for the last 2 and a half million years have greatly influenced the formation of what is now known as Wisconsin .Wisconsin is a northern mid-west state in the USA. These changes were caused by changes in the earth’s orbit and axis. Colder periods during this time frame caused much of the northern hemisphere to be covered in glaciers. There have been warmer periods like the present during this period. The Wisconsin glaciation was the last glacial expansion and cooling cycle. Around 26,000 years ago the glacier moved into what is now known as Wisconsin. For 10,000 years it expanded before again warming. The ice finally melted away from after another 6,000 years the last glacier was named the Lauren tide ice sheet. It was shaped partly by the land. High lands created lobes of ice. One of the lobes flowed down Lake Michigan Superior lobes were in Northern Wisconsin. The Green bay lobe flowed in the lowland of green bay into the devils lake gorge. Melt water flowing from it greatly altered the landscape of Wisconsin. The Wisconsin glaciation is different than glaciation experienced by other areas. Erosion in other areas has destroyed the very irregular landscape of Wisconsin is a result of the laurentide ice sheet. These landforms include the vast wet lands and many lakes in the state. (Wisconsin Geologic Survey, 2011)

Second Slide
More than 400 million years ago a meteor crashed into Wisconsin .It created the crater known as rock elm disturbance. It is one of the largest of 100 known crater sites in the world. This has created a blue rock formation that is 60 feet high and 150 feet wide. In 1880 gold and diamonds were found in sediment streams from the crater. In 1980 Superior Oil Company looked for gold and only found placer gold. It is believed that the gold may have washed out of glacial material. (University of Wisconsin River Falls, 2009)
Wisconsin does not have an outcrop of quartz like materials found in Wisconsin. Quartz is found mostly in cobbles.in glacial outwash that happened in the Pleistocene era. This has caused glacial tills and gravel deposited by outwash because of glacial erosion. The gravel is the parent material and consists of quartz, rhyolite , and quartzite. Quartz can be found nearly any riverbank or lakeshore in northern Wisconsin. Quartz assemblages are unique and cannot be compared to other assemblages. (Spott, 2005)
There are more than 300 minerals found in Wisconsin. Some unusual minerals in the state are copper found at the Flambue mine which is no longer mining but used for outdoor recreation. The vein of Black chalcocite-rich ore can easily be seen there. Marcasite can be found near Lake Winnebago. Marcasite is also known as white iron ore. The state has many granite mines. A geologic feature containing granite is the weathered (Wisconsin Geologic Survey, 2011) granite at nine mile pluton formed by dikes.
T (Geocaching)hird slide
Red Granite ,natural, igneous rock with a visible crystalline texture is essentially formed of quartz and orthoclase or microcline it is very hard the chemical composition of granite is feldspar -65% to 90% quartz -10% to 60% while that of biotite - 10% and 15%. Silica (SiO2) : 70 - 77 % Alumina (Al2O3) : 11 - 14 % Potassium Oxide (P2O5) : 3 - 5 % Soda (Na2O) : 3 - 5 % Lime : 1 Iron (Fe2O3) : 1 - 2 % Iron (FeO) : 1 - 3 % Magnesia (Mg) : 0.5 - 1 % Titina : Less than 1 % (0.38 %) Water (H2O) : 0.03 % Granite is mined from the ground using blasting and digging. Red Granite is used in construction and countertops. ( Geology Museum , 2005)
Fourth slide

Fourth slide
The oldest rocks are Arechean they are 2800 million years old and are found in Wood county Ages that are the same as these have been found also in Hurley County. The rocks dated include volcanic rocks, 2’700 year old granite, shale and gneisses. These rocks are pre Cambrian sedimentary rocks cover northern Wisconsin with volcanic rock found in the center of the state. (UW extension, 2006 ) The geologic time scale allows us to use fossils to date Wisconsin another method of dating used is radioactive testing this is where the heat is measured from radioactive decay giving an absolute age. Radioactive elements are unstable atoms that give off particles. Emitting these particles transforms the unstable atoms into different, more stable elements. This is called radioactive decay, and it occurs at a constant rate specific to each isotope (of, 2011)
Fifth slide
An important feature geologically of Wisconsin is the Waukesha fault. During the post penokean event Southern Wisconsin underwent changes that put in place granite and rhyolite. Events that happened after this during plutonic events caused rhyolite dike to intrude into the Precambrian basement. The Waukesha fault is not completely understood by scientists. It is believed to be much more complex than what was once thought. The use of geophysical techniques may help discover new information about the fault. Most studies of the fault show it is high angle fault. It is believed that a second fault much younger runs close to the Waukesha fault. Scientists believe the basin formed do to lithospheric compression while under a diapiric load. There is no absolute single origin to fully explain the Michigan basins formation. Because the fault goes through all Paleozoic sediment but not the glacial till glacial rebounding does not seem likely cause of the faulting. More studies are needed to understand this fault. (James M. Robertson, 2005)
Sixth slide
An interesting feature of Wisconsin that has much to do with the rock cycle is the Baraboo Ranges they are located in south-central Wisconsin and are a oval ring of hills, approximately 30 miles long and 10 miles wide. The oval range is made of a metamorphic rock the Baraboo Quartzite. While natural forces of erosion have stripped layers of rock from the range over the past 350 million years quartzite is a tough rock. The rock cycle involves rocks changing as erosion and different processes change rocks. IN this case erosion caused the features. During this process the rocks are turned into different rocks through metamorphosis. Originally quartz grains formed sandstone a sedimentary rock. The sand stone eroded from the Penokean Mountains which were located north of the range and existed in the Proterozoic eon. The sandstone was then laid down over the following 200 million years. The Baraboo quartzite is metamorphosed sandstone. (Montgomery) Granite is the most plentiful igneous rock in this district.

Seventh slide
In central Wisconsin many features can be seen that cannot be seen anywhere else east of the Mississippi in the U.S.A. These features include rocky hills, towers of sandstone, steep slopes and bluffs. These unusual landforms are erosion that has taken place that was not glaciation. The glacier moved over northwest and northeast Wisconsin. The areas affected by the glacier moving over them lost most if not all of these interesting rock features. Also glacial lakes are seen in areas where the glacier moved across the land digging out the glacial lakes these are not seen in the drift less area. Erosion in the drift less area is wind and water erosion not glaciation. (Martin, 1995-2012)

Eighth slide
Wisconsin has many geological features including sandstone mesas in the central region of the state. Swamps and marshes that cover vast amounts of land in the state. Lake Michigan the only great lake completely in the United States, Many glacial caves exists. The cave of the mounds was formed around 2 million years ago it is the most significant cave in the mid-west. The rock it is formed from is limestone. The rock dates back 400 million years to the Ordovician period. During the areas warm period a large warm sea covered the area. The cave of the mounds was once completely submerged beneath the water. As water seeped through the rock it formed carbonic acid which slowly ate the rock allowing more and more water to stream through the rock which eroded it more. Eventually the water level lowered and the mound was above ground and no longer filled water but with air. As surface water seeped through the earth’s soil and then through the limestone Calcium carbonate trickled through the cave as the water evaporate calcite crystals formed on the ceiling of the cave. (Cave of the Mounds National Natural Landmark & www.caveofthemounds.com, 2011) Slide 9
I chose Wisconsin because of its unique features. In many ways it is very different than other Midwestern states. I am a Wisconsinite so I thought it would be exciting to learn more about the states geological features. I have always wondered why Wisconsin’s landscape is so varied. I have also wondered why we have sandstone pillars that look like they belong in the desert not in a northern state. I found that glaciation is why we have such a unique landscape. I also learned that part of central Wisconsin was a drift less area that the glacier did not move over. I was surprised by how interesting the state is geologically. I learned about the Baraboo rock outcrop which is one of the oldest in North America. The glacial lakes were interesting to read about. I also thought the cave of the mound one of the largest caves in the Midwest very fascinating. I think after doing this report I can never say I live in an uninteresting state.
Bibliography
Geology Museum . (2005). Minerals found in Wisconsin. Retrieved from Geology and Paleontology of Wisconsin : http://www.geology.wisc.edu/~museum/wiscgeopaleo.htm
Cave of the Mounds National Natural Landmark & www.caveofthemounds.com. (2011). Science of the Cave. Retrieved from cave of the mounds: http://www.caveofthemounds.com/about.htm#science
Geocaching. Rock Elm Disturbance . Impact Zone. /Mineralogy, University of Wisconsin, River Falls.
Geology of Ice Age National Scientific Reserve of Wisconsin. (n.d.). Ice Age. Retrieved from Geology of Ice Age National Scientific Reserve of Wisconsin: http://www.nps.gov/history/history/online_books/science/2/chap1.htm
James M. Robertson, S. M. (2005). The Waukesha Fault and Its Relationship to the Michigan Basin. Retrieved from UW Extension: http://wisconsingeologicalsurvey.org/wofrs/WOFR2005-05.pdf
Martin, L. (1995-2012). The central plain of wisconsin. Retrieved from wisconsin online: http://www.wisconline.com/wisconsin/geoprovinces/centralplain.html
Montgomery, K. (n.d.). The Baraboo Ranges and Devil's Lake Gorge. Retrieved from Department of Geography-Geology : http://www.marathon.uwc.edu/geography/baraboo/baraboo.htm of, D. (2011, 9 29). Foundational Concepts. Retrieved from “Smithsonian”: http://paleobiology.si.edu/geotime
Spott, E. (2005). ANALYSIS OF QUARTZ IN NORTHERN WISCONSIN: DEFICIENCIES, MISCONCEPTIONS. Retrieved from Nebraska Anthropologis: http://digitalcommons.unl.edu/cgi/viewcontent.cgi?article
University of Wisconsin River Falls. (2009, march 14). Rock Elm Asteroid Crater Site of Speculation, Study. Retrieved from University of Wisconsin River Falls: 2009
UW extension. (2006 , April). GEOLOGIC HISTORY OF WISCONSIN’S BEDROCK. Retrieved from Wisconsin Geological and Natural History Survey: http://wisconsingeologicalsurvey.org/pdfs/pgszpdf/bedrock_geology.pdf
Wisconsin Geologic Survey. (2011, December 12). Climate Change-The long View. Retrieved from Wisconsin Geological and Natural History Survey: http//wisconsingeologicsurvey.org

Bibliography
Geology Museum . (2005). Minerals found in Wisconsin. Retrieved from Geology and Paleontology of Wisconsin : http://www.geology.wisc.edu/~museum/wiscgeopaleo.htm
Cave of the Mounds National Natural Landmark & www.caveofthemounds.com. (2011). Science of the Cave. Retrieved from cave of the mounds: http://www.caveofthemounds.com/about.htm#science
Geocaching. Rock Elm Disturbance . Impact Zone. /Mineralogy, University of Wisconsin, River Falls.
Geology of Ice Age National Scientific Reserve of Wisconsin. (n.d.). Ice Age. Retrieved from Geology of Ice Age National Scientific Reserve of Wisconsin: http://www.nps.gov/history/history/online_books/science/2/chap1.htm
James M. Robertson, S. M. (2005). The Waukesha Fault and Its Relationship to the Michigan Basin. Retrieved from UW Extension: http://wisconsingeologicalsurvey.org/wofrs/WOFR2005-05.pdf
Martin, L. (1995-2012). The central plain of wisconsin. Retrieved from wisconsin online: http://www.wisconline.com/wisconsin/geoprovinces/centralplain.html
Montgomery, K. (n.d.). The Baraboo Ranges and Devil's Lake Gorge. Retrieved from Department of Geography-Geology : http://www.marathon.uwc.edu/geography/baraboo/baraboo.htm of, D. (2011, 9 29). Foundational Concepts. Retrieved from “Smithsonian”: http://paleobiology.si.edu/geotime
Spott, E. (2005). ANALYSIS OF QUARTZ IN NORTHERN WISCONSIN: DEFICIENCIES, MISCONCEPTIONS. Retrieved from Nebraska Anthropologis: http://digitalcommons.unl.edu/cgi/viewcontent.cgi?article
University of Wisconsin River Falls. (2009, march 14). Rock Elm Asteroid Crater Site of Speculation, Study. Retrieved from University of Wisconsin River Falls: 2009
UW extension. (2006 , April). GEOLOGIC HISTORY OF WISCONSIN’S BEDROCK. Retrieved from Wisconsin Geological and Natural History Survey: http://wisconsingeologicalsurvey.org/pdfs/pgszpdf/bedrock_geology.pdf
Wisconsin Geologic Survey. (2011, December 12). Climate Change-The long View. Retrieved from Wisconsin Geological and Natural History Survey: http//wisconsingeologicsurvey.org

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...Project 2 The Glomar Challenger was a deep sea research and scientific drilling vessel for oceanography and marine geology studies. The JOIDES Resolution (Joint Oceanographic Institutions for Deep Earth Sampling) is a scientific drilling ship. The JOIDES Resolution was the successor of Glomar Challenger. Both vessels would drill and take core samples at specific locations. The samples were used to determine the paleontologic and isotopic dating studies, thus providing conclusive evidence of seafloor spreading hypothesis and plate tectonics. Most earthquakes and volcanic eruptions do not strike randomly but occur in specific areas, such as along plate boundaries. One such area is the circum-Pacific Ring of Fire, where the Pacific Plate meets many surrounding plates. The Ring of Fire is the most seismically and volcanically active zone in the world. The most earthquakes in Europe occur in the collision zone of Eurasian and African plates. The Mediterranean regions where countries like Turkey, Greece, and Italy are located are where the majority of earthquakes in Europe occur. In 1977 scientists discovered hot springs at a depth of 2.5 km, on the Galapagos Rift which is off the coast of Ecuador. It is remarkable that these hot springs can be as hot as 380 degrees Celsius and are home to some of the earth’s most diverse ecosystems in the world. This ecosystem is sustained not by the suns energy but by chemosynthesis. Four types of plate boundaries: A destructive...

Words: 375 - Pages: 2

Premium Essay

Geology

...Victor Manevich 02/25/10 Geology 100 * What are Glomar Challenger and JOIDES Resolution? What do they do? The Glomar Challenger was the first research ship explicitly engineered to drill and collect core samples from the deep ocean floor. The JOIDES Resolution ship was engineered for the same purpose as the Glomar Challenger. The JOIDES Resolution was completed in the 1990s and has more advanced and precise technology than the Glomar Challenger, which was completed in the 1960s. The JOIDES Resolution ship is able to drill far deeper into the ocean floor than the Glomar Challenger. * Using the maps and diagrams on the Web site, where are the major concentrations of the world's earthquakes? Where are most earthquakes in Europe? The major concentrations of the world’s earthquakes occur in countries, which are near the Ring of Fire in the Pacific Ocean. The most earthquakes in Europe occur in the collision zone of Eurasian and African plates. The Mediterranean regions where countries like Turkey, Greece, and Italy are located are where the majority of earthquakes in Europe occur. * What undersea hot springs were discovered in 1977? What is remarkable about these (and other) undersea hot springs? On the Galapagos Rift off the coast of Ecuador scientist discovered hot springs at a depth of 2.5 kilometers. It is remarkable that these hot springs can be as hot as 380 degrees Celsius and are home to some of the earth’s most diverse ecosystems in the world. This ecosystem...

Words: 554 - Pages: 3