Quiz 2 week #7

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El Paso Community College *

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Geology

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Dec 6, 2023

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QUIZ #2. Answer all questions and turn in on Blackboard. What is your name? Elmer Saenz 1. (1 point) Which of the three main classes of stress would cause the clay layers to deform this way? Compressional Stress 2. What is the name of the structure shown in the image below, inside the black circle drawn onto the photograph? (1 point)
Anticline Structure 3. (6 points, one point per row) Fill in the chart below. It compares types of plate boundaries with the features and common hazards found there. You can mark an X in each box where it applies. (For example, if there are earthquakes at a boundary where two oceanic plates diverge, mark an X in that box) Two oceanic plates converge Two oceanic plates diverge Two continental plates converge Two continental plates diverge An oceanic plate and a continental plate converge Two plates slide past each other Earthquakes x x x x x x Tsunamis x x Volcanoes x x Mountains that aren’t volcanoes x x Ridge made of volcanoes in the ocean x
Deep trench in the ocean x 3. Volcano Scenario Volcano X is a very active volcano in Central America. It is formed by the subduction of the Cocos Plate under the Caribbean Plate. Rock layers on this large, steep sided (steeply sloping) volcano have been identified as andesite, which is relatively high in viscosity. The seismic activity at Volcano X has been increasing in frequency, intensity and magnitude. Scientists are concerned that an eruption may be imminent. Because of your knowledge of earth science, your friend who lives about 20 kilometers from the volcano has asked you for advice. They want to know some things about Volcano X and what types of hazards they may expect from Volcano X. A (1 point). What type of volcano (think of the three main classes of volcanoes) is Volcano X? Explain your reasoning (need explanation for full credit). ( Volcano X is a composite or stratovolcanoe . Composite volcanoes are also known as stratovolcanoes or stratocones. They are the most common type of volcano and are formed by the eruption of viscous lava and ash. Composite volcanoes are typically steep-sided and conical in shape, with a central vent. Volcano X is described as being steep-sided and having erupted andesite lava. Andesite is a type of lava that is relatively high in silica, which makes it viscous. This suggests that Volcano X is a composite volcano.) B (1 point). It is stated above that the Volcano X region is characterized by the subduction of the Cocos Plate under the Caribbean plate. Given that it represents a subduction zone, which of the following observations would be most likely to happen in regards to the faults in the region when earthquakes happen on them? (a) Hanging wall moves up (b) Hanging wall drops down (c) Hanging wall and footwall move side-to-side laterally with regards to each other. D. (1 point per answer) Your friend asks you which types of volcanic hazards they should prepare for from this volcano. Answer yes or no for each item below BUT ALSO EXPLAIN YOUR REASONING (you must give an explanation for full credit). 1. Volcanic ash clouds in the sky and falling out over the area Yes . Composite volcanoes are known for producing explosive eruptions that can generate large ash clouds. Ash clouds can travel long distances and can cause a number of hazards, including respiratory problems, damage to crops and infrastructure, and disruptions to air travel. 2. Smooth, very liquid, black lava flows running down from the mountain No . Composite volcanoes typically erupt viscous lava that does not flow very easily. This type of lava is more likely to form lava domes and pyroclastic flows, which are fast-moving mixtures of hot gas and rock. 3. Explosive eruption blast
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Yes . Composite volcanoes are known for producing explosive eruptions. Explosive eruptions can generate powerful shockwaves and pyroclastic flows. 4. The image below, obtained near the bottom of the Grand Canyon, shows a quartz vein that has been deformed. (a) (1 point) Which class of deformation caused the quartz vein to change shape? The quartz vein in the image shows evidence of ductile deformation . This is because the quartz has been stretched and folded into a curved shape, without breaking. Ductile deformation occurs when rocks are subjected to high temperatures and pressures over a long period of time. This causes the rocks to become more pliable and less likely to break. (b) (1 point) Did this deformation most likely occur near Earth’s surface or deep inside the Earth? The fact that the quartz vein has been deformed I think this suggests that it was subjected to high temperatures and pressures at some point in its history. This is more likely to have happened at great depth, where the rocks are hotter and under more pressure. Therefore, the deformation of the quartz vein most likely occurred at great depth. 5. The cartoon below, from your book, illustrates the tectonic setting of East Africa. For 1 point, what class of plate boundary/plate margin formed these structures? Be as specific as possible. In summary, it is mostly understood that the East African Rift Valley was formed due to the pulling apart of the African Plate and the Somali Plate along a divergent plate boundary . This process led to the gradual thinning of the lithosphere, upwelling of magma, and the creation of new crust, resulting in the unique geological features we can observe in the picture. 6. (1 point) An earthquake strikes El Paso one morning at 7 AM! The city shakes, items are thrown off of shelves, and cracks appear in some houses. It seems to be the only thing that people want to talk
about. Later that day, you see several friends of yours and everyone discusses the earthquake. One of them says, “Yeah, they said that here on the far east side it was 4 on the Richter scale, it was a big shake but not too bad, but I hear the worst damage was up by Transmountain, over there it hit magnitude 6.” What was incorrect about your friend’s statement? Explain. I think my friend’s statement was incorrect because the Richter scale is not a measure of the intensity of an earthquake at different locations, but a measure of the magnitude of an earthquake at wherever it was. The magnitude is the same for all locations, but the intensity may vary depending on the distance from the epicenter, the local geology, and other well known factors.