Axia College Material Appendix L Week Six Lab Report: Metamorphic Rocks Answer the lab questions for this week and summarize the lab experience using this form. Full Name Date Carefully read pages 108-116 of Geoscience Laboratory. Complete this week’s lab by filling in your responses to the questions from Geoscience Laboratory. Select answers are provided for you in red font to assist you with your lab work. Although you are only required to respond to the questions in this worksheet
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Due to the discovery of shock metamorphism rocks (suevite breccia) and melted original rocks scattering in the southern area of Bukit Bunuh‚ it was suspected that the area had the possibility of being impacted by meteorite. The founded boulders made the archaeologists from the Centre for Global Archaeological Research (CGAR) of Universiti Sains Malaysia (USM) to propose of the possibility of Bukit Bunuh as a meteorite impact site. This proposal was led to intense research in the area by utilizing
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Photographer’s Choice RF/ Getty Images The Earth’s crust is an extremely thin layer of rock‚ like the skin of an apple in relative terms. It amounts to less than half of 1 percent of the planet. But the crust is exceptionally important‚ and not just because we live on it. The crust can be thicker than 80 kilometers in some spots‚ less than one kilometer in others. Underneath it is the mantle‚ a layer of rock some 2700 kilometers thick that accounts for the bulk of the Earth. The crust is primarily
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starts 1.7 billion years ago with the Idaho Springs gneiss found at the upper parking lot of Red Rocks Amphitheater. This rock is made up of potassium feldspar and quartz predominantly‚ which makes the rock appear mostly white in color‚ however‚ hematite stains the outside to give it a red color. The Idaho Springs gneiss was created by two geological events‚ both the growing of the North American basement rock and the formation of super continent Columbia. This can be seen because the Idaho Springs gneiss
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clumps held together by static charge. -These mineral grains grew into small pieces of rock orbiting the sun -over the next few million years some of these rocks collided and grew bigger -when a rock grew to become around half a mile across‚ its gravitational pull became strong enough to pull objects towards it. (The bigger the rock was the faster it grew because it had higher gravitational pull) -so that biggest rock eventually grew to become ‘the fledgling earth’ -soon this small planet grew to attract
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The Great Smoky Mountains The Great Smoky Mountains landform is mostly sedimentary rocks that were formed by the accumulation of sand‚ clay‚ silt‚ sand‚ gravel‚ and minor amounts of calcium carbonate in flat-lying layers. According to The Great Smoky Mountain’s website‚ about 545 million years ago the sediments were formed and large amounts of those sediments were washed down into lowland basins from adjacent highlands. The colliding between the edge of the North American tectonic plate and the
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On the Digermulen Peninsula‚ the succession starts with the classic Neoproterozoic glacial tillite of the Mortensnes Formation (Fig. 3). This tillite has traditionally been tentatively correlated by many workers (e.g.‚ Rice et al. 2011‚ and references therein) with the type ’Gaskiers’ glaciogenic succession in Newfoundland‚ which is between 584 and 582 Ma old‚ based on zircon U–Pb ages from intercalated ash beds (Bowring et al. 2002). The Mortensnes Formation is separated downwards from the ’Marinoan’
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state. (1980‚ April). Retrieved from http://vulcan.wr.usgs.gov/LivingWith/VolcanicPast/Places/volcanic_past_washington_state.html 2. Kamiak butte summit - washington mountain peak information. (2006). Retrieved from http://www.summitpost.org/mountain/rock/640640/kamiak-butte.html 3. Kamiak butte summit - washington mountain peak information. (n.d.). Retrieved from http://www.mountainzone.com/mountains/detail.asp?fid=3962156 4. Peters‚ E.K. (n.d.). Geological field trip 1: from opans and ancient mountaintops
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modes associated with them‚such as symmetric and asymmetric stretches‚bends‚ rocks‚ and tortional modes. For MRZ‚ the C-H stretching Vibrations are observed at 3057‚ 3043‚ 3016 and 2999 cm-1. The asymmetric and symmetric stretching bands of CH2 are observed in the range from 2900 to 2700 cm-1 and this stretching band is mainly coupled with the CH3 stretching vibration. Mirtazapine has only one CH3 group. The C-H stretching vibrations of methyl are observed between 3000 and 2900 cm-1. A methyl group
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depression. It is located at the contact between cretaceous and Eocene deposits. One of the early geologic works was carried out by Ball and Beadnell (1903). They produce a topographical- geological map of the oasis and discuss the stratigraphy of the rock exposed. They distinguished three topographic features; the bounding escarpments; the conical hills within the depression and the oasis floor. They notice that the southern scarp is steeper than the northern scarp. The eastern scarp has smooth outline
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