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2004 Physical Geology 1st Exam sample

Course: GEOS 211, Fall 2009
School: Earlham
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211, Geology Physical Geology First Exam February 5, 2004 Name PART 1: Multiple choice: (60 points) Please circle the letter that best answers or completes the question. 1. Which boundary is the surface upon which lithospheric plates move? A. The Mohorovicic Discontinuity (the Moho) B. The asthenosphere lithosphere boundary C. Gutenberg's Discontinuity D. The crust The average geothermal gradient in Earth's...

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211, Geology Physical Geology First Exam February 5, 2004 Name PART 1: Multiple choice: (60 points) Please circle the letter that best answers or completes the question. 1. Which boundary is the surface upon which lithospheric plates move? A. The Mohorovicic Discontinuity (the Moho) B. The asthenosphere lithosphere boundary C. Gutenberg's Discontinuity D. The crust The average geothermal gradient in Earth's crust is which of the following? A. 25C/km B. 35C/km C. 45C/km D. 15C/km The basic structural unit in all silicate minerals is the... A. Polymorph B. Metallic bond C. Silicate tetrahedron D. Chloride ion The core of Earth consists of ________. A. A solid inner and a solid outer component B. A solid outer and a liquid inner component C. A liquid inner and a liquid outer component D. A solid inner and a liquid outer component As compared to aphanitic igneous rocks, phaneritic rocks ________. A. Cooled more rapidly B. Cooled less rapidly C. Are still molten D. Aren't cool Which of the following controls the viscosity of erupting lavas? A. Si02 content B. K20 content C. Al203 content D. Mg0 content. What best explains seamount guyot tracks across an expanse of ocean A. Motion of a hot spot beneath continental lithosphere B. Motion of oceanic lithosphere over a stationary hot spot C. Ancient astronauts D. An ancient mid-ocean ridge 2. 6. 7. 8. 9. 10. Page 1 Geology 211, Physical Geology First Exam February 5, 2004 11. Name Submarine mafic eruptions commonly exhibit _____________. A. Porphyritic textures B. Lava fountains C. Pillow structures D. Columnar joints. Igneous intrusions which cut across layered strata are termed _____________. A. Sills B. Batholiths C. Laccoliths D. Dikes. The Heliocentric theory of the solar system was championed by whom? A. Copernicus B. Ptolemy C. Eratosthenes D. Newton Where would geothermal heat flow be expected to be low? A. Along mid-ocean ridges B. At a hot spot C. At the base of the lithosphere D. In the center of a continent What discovery was made upon visiting the Mid-Atlantic Ridge in the research submersible "Alvin"? A. Pillow basalts B. Rift valleys C. An ecosystem based on energy from hot mineralized water D. The singing group "the Chipmunks" At a triple junction is a place on Earth's surface where ________. A. Three tectonic plate boundaries coincide B. Igneous, metamorphic and sedimentary rocks coexist C. Glacial ice, continental rocks, and oceanic rocks can be found together D. Three phases of matter (solid, liquid and gas) occur together in equilibrium A cross-section through the oceanic crust that is preserved on continental crust is term a(n)________. A. Gabbro B. Pillow basalt C. Sheeted dike complex D. Ophiolite 12. 13. 14. 15. 16. 17. Page 2 Geology 211, Physical Geology First Exam February 5, 2004 18. Name Which tectonic feature corresponds with the deepest part of the ocean? A. A mid-ocean ridge B. A transform fault fracture zone C. A continent continent collision D. A subduction trench What can a geologist interpret from a xenolith? A. The type of country rock a magma passed through B. The temperature of the magma C. The pressure of the magma D. Ancient warrior princesses had kidney stones Which of the following characterizes the transform fault that offsets mid-ocean ridge segments? A. An abundance of shallow earthquakes B. Effusive volcanism C. All of the above D. All of the below Continental crust and oceanic crust ________. A. Never occur on the same tectonic plate B. Can transition one into the other C. Are really the same D. Always transition one into the other X-Ray diffraction is useful in the study of minerals because it allows scientists to ________. A. Determine that a mineral is solid B. Determine that a mineral is naturally occurring C. Determine that a mineral has an ordered atomic structure D. Determine that a mineral is inorganic A laccolith is ________. A. A horizontal tabular intrusion that lies parallel to surrounding layers of sedimentary rock B. A mushroom-shaped igneous intrusion C. An intrusion formed within the magma chamber of a volcano D. A vertical tabular intrusion that cuts across preexisting layers Natural glass is not considered a mineral because it ________. A. Is not homogenous B. Is organic C. Does not have a fixed crystalline structure D. Can be made synthetically as well as being a naturally occurring substance 19. 20. 21. 22. 23. 24. Page 3 Geology 211, Physical Geology First Exam February 5, 2004 25. Name How does magma composition relate to volcanic eruptive style? A. Thick viscous magmas erupt in mild runny lava flows B. was replaced by the theory of plate tectonics C. was incorporated within the theory of plate tectonics D. Thick viscous magmas erupt in massive explosions of rock and ash. Which is the most common rock-forming mineral group in Earth's crust? A. Calcite B. Quartz C. Feldspars D. Clay minerals The oldest oceanic crust on the sea floor occurs ________. A. At the edges of ocean basins B. In volcanic island arcs C. Near mid-ocean ridges D. Randomly distributed over the entire ocean basin Silica tetrahedra may be coordinated to form all of the following structures EXCEPT ________. A. Long single chains B. Extensive two-dimensional sheets C. Three-dimensional frameworks D. Double helixes A(n) __________ is formed of material scraped off a descending, lithospheric plate. A. Mass movement complex B. Continental shelf, terrain complex C. Accretionary-wedge complex D. Subterranean-accumulation complex A good example of a present-day, passive continental margin is the __________. A. North flank of the East Pacific Rise B. West coast of South America C. East coast of the Japanese Islands D. West coast of Africa 26. 27. 28. 29. 30. Page 4 Geology 211, Physical Geology First Exam February 5, 2004 31. Name Earth's surface is protected from solar wind and cosmic radiation by ________. A. Earth's gravitational field B. The ozone layer C. Omniscient beings D. The Van Allen radiation belts Wegener's idea of continental drift was supported the following lines of evidence ________. EXCEPT A. Fossils of non-swimming organisms were found on opposite sides of the Atlantic B. Mountain belts and unique rock types were observed to link across the Atlantic C. The distribution of glacial striations and tropical sediments were consistent with Pangea D. Paleomagnetic positive and negative anomalies (stripes) preserved in the oceanic crust What is a guyot? A. A circular feature formed by impact of an asteroid on continental crust B. A flat-topped submarine volcano C. A blob-like igneous rock body that has cooled beneath the surface of the Earth D. A mushroom-shaped igneous intrusion Continental crust ________. A. Is thinner than oceanic crust B. Contains more mafic rocks than oceanic crust C. Is less dense than oceanic crust D. Is mostly basaltic in composition What does Bowen's Reaction Series describe? A. Temperature changes in a cooling magma B. Pressure changes in a cooling magma C. Compositional changes in a cooling magma D. Textural changes in a cooling magma Which of the following descriptors characterizes tectonic plates? A. They are rigid B. They are thin and hot C. They are made of continental rocks which plow through weaker oceanic rocks D. They behave like plastic solids 32. 33. 34. 35. 36. Page 5 Geology 211, Physical Geology First Exam February 5, 2004 Name 37. How does magma composition relate to volcanic eruptive style? A. Increasing silica content makes magmas less viscous leading to less violent eruptions B. Decreasing silica content makes magmas less viscous leading to less violent eruptions C. Increasing silica content makes magmas more viscous leading to less violent eruptions D. Decreasing silica content makes magmas less viscous leading to more violent eruptions What is the most abundant element in the crust? A. Silicate B. Iron C. Oxygen D. Aluminum One difference between lava and magma is that ________. A. Magma is cooler B. Magma is more dense C. Lava has lost volatiles D. Lava is under greater pressure Minerals that lack cleavage are said to have ________. A. A poor attention span B. Ductility C. High specific gravity D. Fracture What is a major difference between a ridge transform and a fracture zone? A. Unlike a fracture zone, oceanic crust at a transform travels in 2 directions. B. Fracture zones have multiple shallow earthquakes; transforms don't C. Fracture zones are thermally expanded; transforms aren't D. Transforms have extensive volcanic activity unlike fracture zones At a subduction zone, which of the following is NOT present? A. A volcanic arc B. A bathymetric trench C. An axial rift D. An accretionary wedge Which of the following discoveries was the result of submarine detection efforts during the Cold War? A. Sonic booms create clouds. B. Earthquakes concentrate along Mid-Ocean Ridges and ridge transform offsets. C. Magnetic stripes were found oriented perpendicular to the Mid-Ocean Ridges. D. Sea-water is a poor transmitter of sound waves. 38. 39. 40. 41. 42. 43. Page 6 Geology 211, Physical Geology First Exam February 5, 2004 44. Name Coarse-grained granite is most similar in composition to fine-grained ________. A. Andesite B. Basalt C. Komatiite D. Rhyolite Which of the following is an inference you can make about any euhedral quartz crystal? A. The crystal has magical healing powers B. The crystal is a polymorph C. The crystal must have grown in an open space D. The crystal must be from Herkimer, New York 45. Part 2, Short Answer: (20 points) Please write a short sentence to answer the question 46. What is the Wadati Benioff Zone? 47. Who first proposed continental drift? 48. What is a black smoker? 49. What does mag...

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Harvard - MM - 545
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Harvard - MM - 545
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Harvard - MM - 545
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Harvard - MM - 545
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Harvard - MM - 545
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Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] 0.000 197.858 106.781 -71.373 41.869 -72.971 43.203 15.756 -72.172 42.536 67.669 -60.000 243.575 131.454 -72.951 43.4
Harvard - MM - 545
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Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] 0.000 197.911 106.810 -73.197 43.006 -71.147 42.065 15.560 -72.172 42.536 67.669 -60.000 191.635 103.423 -73.197 42.9
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] 0.000 197.884 106.795 -72.961 41.862 -71.383 43.209 15.661 -72.172 42.536 67.669 -60.000 194.533 104.987 -72.963 41.9
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] 0.000 198.289 107.014 -73.260 42.145 -71.084 42.927 14.090 -72.172 42.536 67.669 -60.000 197.839 106.771 -73.220 42.1
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] 0.000 197.824 106.763 -72.985 43.193 -71.359 41.878 15.879 -72.172 42.536 67.669 -60.000 202.041 109.039 -72.995 43.2
Harvard - MM - 545
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Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] 0.000 198.060 106.891 -71.441 41.827 -72.903 43.245 14.996 -72.172 42.536 67.669 -60.000 197.090 106.367 -72.865 43.2
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] 0.000 199.736 107.795 -71.931 41.655 -72.413 43.416 5.545 -72.172 42.536 67.669 -60.000 217.002 117.113 -72.242 41.6
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] 0.000 198.045 106.882 -72.908 41.829 -71.436 43.242 15.056 -72.172 42.536 67.669 -60.000 198.172 106.951 -72.601 41.7
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] 0.000 199.868 107.866 -73.385 42.628 -70.959 42.444 3.916 -72.172 42.536 67.669 -60.000 215.709 116.415 -73.519 42.3
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 197.691 106.691 -73.088 43.115 -71.256 41.957 16.353 -72.172 42.536 67.669 4V8 1B9
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.058 106.889 -73.226 42.971 -71.118 42.1 15.005 -72.172 42.536 67.669 DDH OWD
Harvard - MM - 545
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Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.374 107.6 -73.355 42.744 -70.989 42.327 8.534 -72.172 42.536 67.669 DDH BOS
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.156 106.942 -73.242 42.12 -71.102 42.951 14.623 -72.172 42.536 67.669 GBR LWM
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.596 107.18 -73.294 42.874 -71.05 42.197 12.765 -72.172 42.536 67.669 DDH OWD
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.006 107.401 -73.329 42.808 -71.015 42.264 10.748 -72.172 42.536 67.669 DDH BOS
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.54 107.15 -73.288 42.883 -71.056 42.188 13.016 -72.172 42.536 67.669 DDH OWD ORE GDM
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.12 106.923 -73.236 42.959 -71.108 42.113 14.766 -72.172 42.536 67.669 DDH OWD
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.04 106.879 -73.223 42.975 -71.121 42.096 15.076 -72.172 42.536 67.669 DDH OWD ORE GDM
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 200 107.937 -73.392 42.539 -70.952 42.532 0.148 -72.172 42.536 67.669 PSF BVY
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.618 107.192 -73.296 42.201 -71.048 42.87 12.667 -72.172 42.536 67.669 GBR LWM
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.073 107.437 -73.334 42.275 -71.01 42.797 10.381 -72.172 42.536 67.669 GBR LWM
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.985 107.929 -73.392 42.504 -70.952 42.567 1.338 -72.172 42.536 67.669 PSF BVY ORE ORE
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.237 106.986 -73.253 42.135 -71.091 42.936 14.3 -72.172 42.536 67.669 GBR LWM ORE GDM
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.865 107.325 -73.318 42.831 -71.026 42.241 11.485 -72.172 42.536 67.669 DDH OWD
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 197.865 106.785 -73.186 43.019 -71.158 42.053 15.728 -72.172 42.536 67.669 DDH 1B9
Harvard - MM - 545
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Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.789 107.823 -73.381 42.418 -70.963 42.653 4.96 -72.172 42.536 67.669 PSF BVY ORE ORE
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.029 107.413 -73.331 42.804 -71.013 42.268 10.624 -72.172 42.536 67.669 DDH BOS
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.883 107.874 -73.386 42.622 -70.958 42.449 3.688 -72.172 42.536 67.669 PSF BOS ORE ORE
Harvard - MM - 545
<?xml version="1.0" encoding="UTF-8"?><Error><Code>NoSuchKey</Code><Message>The specified key does not exist.</Message><Key>943b6b2a28f57a16e8cf45f11a2b415258498429.txt</Key><RequestId>A88BD4E3894E1E6C</RequestId><HostId>ttK43XX543rDwqGfKWk5I8keBmxZ
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.641 107.744 -71.891 41.662 -72.453 43.409 6.462 -72.172 42.536 67.669 5B3 CNH
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.964 107.918 -72.084 41.639 -72.26 43.433 2.054 -72.172 42.536 67.669 IJD CNH
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.839 107.851 -72.359 41.648 -71.985 43.424 4.332 -72.172 42.536 67.669 IJD CNH ORE GDM
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.096 107.45 -71.714 41.706 -72.63 43.365 10.251 -72.172 42.536 67.669 5B3 VSF ORE GDM
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.89 107.878 -72.326 41.644 -72.018 43.427 3.572 -72.172 42.536 67.669 IJD CNH ORE GDM
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 197.889 106.798 -73.192 42.06 -71.152 43.012 15.641 -72.172 42.536 67.669 GBR MHT GDM ORE
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 197.805 106.753 -72.993 41.884 -71.351 43.188 15.948 -72.172 42.536 67.669 BDL CON ORE GDM
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.041 106.88 -73.223 42.975 -71.121 42.096 15.07 -72.172 42.536 67.669 DDH OWD
Harvard - MM - 545
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Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.054 107.427 -71.703 41.71 -72.641 43.361 10.485 -72.172 42.536 67.669 5B3 VSF
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.572 107.706 -71.864 41.668 -72.48 43.404 7.061 -72.172 42.536 67.669 5B3 VSF
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.99 107.932 -72.218 41.637 -72.126 43.434 1.061 -72.172 42.536 67.669 IJD CNH
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.28 107.009 -73.259 42.928 -71.085 42.143 14.125 -72.172 42.536 67.669 DDH OWD
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.727 107.79 -72.417 41.656 -71.927 43.416 5.639 -72.172 42.536 67.669 HFD CNH
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 197.697 106.694 -73.068 43.131 -71.276 41.941 16.334 -72.172 42.536 67.669 4V8 1B9
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 197.833 106.768 -72.981 43.196 -71.363 41.875 15.846 -72.172 42.536 67.669 4V8 RI9
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.149 106.939 -73.241 42.953 -71.103 42.119 14.651 -72.172 42.536 67.669 DDH OWD ORE GDM
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.931 107.361 -73.323 42.252 -71.021 42.82 11.142 -72.172 42.536 67.669 GBR LWM
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.457 107.105 -72.796 43.3 -71.548 41.771 13.382 -72.172 42.536 67.669 VSF PVD ORE GDM
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.468 107.111 -71.551 41.77 -72.793 43.302 13.334 -72.172 42.536 67.669 PVD VSF
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.995 107.935 -72.205 41.637 -72.139 43.435 0.774 -72.172 42.536 67.669 IJD CNH ORE ORE
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 198.07 106.896 -71.443 41.825 -72.901 43.246 14.959 -72.172 42.536 67.669 RI9 RUT
Harvard - MM - 545
time[min] xsec[km] xsec[nmi] x1.1st y1.1st x2.1st y2.1st xsec2[nmi] ctr.x ctr.y dpease[nmi] arpt1.1st arpt2.1st arpt1.2nd arpt2.2nd0 199.557 107.698 -71.858 41.669 -72.486 43.403 7.18 -72.172 42.536 67.669 5B3 VSF