Earth Science Questions and Answers

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Find earth science questions and answers with clear, step-by-step explanations to help you understand concepts and improve exam performance. These solutions cover topics commonly included in coursework and exams.

Browse earth science practice questions covering areas such as plate movement, weather patterns, ocean processes, and environmental systems. Each answer explains both the concept and the reasoning behind the solution.

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Question:

Earth and Planetary Surface Processes Winter 2017 Problem set 6 Due in class Wed 8 March, 3pm. Office hours 10am-11am, Hinds 467 Monday 6 March (note change in time from 9am). Q1. Plot the expected steady-state pattern (as a function of distance from the crest) of discharge of regolith on a convex hillslope in a climate in which the production rate of regolith is 20 mm/yr. Report your answer in m2/year. If the regolith was 0.8 m thick, what would be the spatial pattern of the mean downslope velocity of the regolith? How would these numbers change if 25% of the mass loss occurred in solution (dissolved in rainwater)? (From Anderson & Anderson) Q2. From Hartley et al., Nature Geoscience, 2011: Seismic reflection profiling between Iceland and the UK shows a drowned landscape that was above sea level 55 Ma. The landscape was cut into mudstones and is now buried beneath >1 km of sediment, plus 700m of water. The landscape (black square in the below figure) was uplifted and then reburied due to the arrival of the head of mantle plume whose “stalk” now fuels volcanism at Iceland: River profiles (gray is data, black is model): What is the slope of the knickpoint marked β? What is the (range of) approximate drainage areas at β? Assuming n=1 in the streampower law (so that knickpoint shape is preserved on retreat), what is the knickpoint retreat rate vAm ? You can assume v = 2.75 Myr-1 and m = 0.5 for this question. Approximately how many years prior to the landscape becoming “drowned” (frozen in shape) was the knickpoint initiated? Refer to Figure 1. Assume the initiation of knickpoint β corresponds to the arrival of the “mushroom head” of the mantle plume, and the drowning of the landscape corresponds to the switch to the modern, narrow “plume tail” configuration. What is the area over which uplift occurred? Assuming the red-circled area was horizontal and below sea level before the plume arrived, what is the volume of uplifted rocks? Assuming the drowned landscape under investigation is representative of the fractional erosion of the uplifted landscape across the whole red-circled area, what is the volume of rocks fluvially eroded in the plume area during the plume event? What is the erosion flux in km3 yr-1? How does this compare to the Holocene pre-dam global sediment flux of 8 km3 yr-1? Q3. In lecture we discussed accumulation of a stable cosmogenic isotope in a rock undergoing exhumation, and we also discussed accumulation of a radioactive cosmogenic isotope in a rock that has no erosion. In this question we will combine exhumation and decay. Assume a production rate of 10Be of 5 atoms/(gram quartz)/yr at the surface, with an e-folding depth of 1 m (so the production rate is 1.84 atoms/(gram quartz)/yr at 1m depth). 10Be decays exponentially with a half-life of 1.4 Myr. Plot the expected concentration of 10Be at the surface, as a function of erosion/exhumation rate, for a quartzite rock. Make sure to consider the endmembers of very slow erosion/exhumation (for which the 10Be concentration will reach equilibrium between production and decay), and the endmember of very fast erosion/exhumation (for which decay is unimportant in setting the 10Be concentration).

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Solution
Homework
6 months ago
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Question:

Part 3: The Geothermal Gradient. An exporiject skill in any career is reading graphi. In this exercise, you will practice this skill by reading the graph that describes how temperature changes with depth in Earth's interior. The curve that describes this change is known as the Geothermal Gradient. The graph below shows the Geothermal Gradient down to about 300 miles. Remember that Earth's center is almost 4,000 miles down, so you are looking at just the very thin eatermost part of the Earth. However, that is where we live and experience all the wild consequences of living on the surface of a planet that is still very hot inside. These consequences include earthquakes and volcanoes. 1. The temperature shown by the arrow under number 1 is _____ degrees Fahrenheit. 2. The depth shown by the arrow next to number 2 is _____ miles below the surface. 3. The temperature shown by the arrow under number 3 is _____ degrees Fahrenheit. 4. Point 4 is a point on the geothermal gradient. This tells us that at 60 miles below the surface, the temperature is _____ degrees Fahrenheit. 5. Point 5 is also a point on the geothermal gradient. It tells us that 100 miles below the surface, the temperature is _____ degrees Fahrenheit. 6. The arrow labelled 6 points to which compositional layer of the Earth? _____ 1. The temperature shown by the arrow under number 1 is _____ degrees Fahrenheit. 2. The depth shown by the arrow next to number 2 is _____ miles below the surface. 3. The temperature shown by the arrow under number 3 is _____ degrees Fahrenheit. 4. Point 4 is a point on the geothermal gradient. This tells us that at 60 miles below the surface, the temperature is _____ degrees Fahrenheit. 5. Point 5 is also a point on the geothermal gradient. It tells us that 100 miles below the surface, the temperature is _____ degrees Fahrenheit. 6. The arrow labelled 6 points to which compositional layer of the Earth? _____ 7. The arrow labelled 7 points to which compositional layer of the Earth? _____ 8. The layer labelled 8 is the _________ the rigid eutermost mechanical layer of the Earth. 9. The layer labelled 9 is the _________ the ductile mechanical layer of the Earth beneath layer 8. 10. Layer 8 is made up of two compositional layers. They are the _____ and the eutermost _____. 11. Layer 9 lies entirely within which layer? _____ 12. Funn though Earth's interior is very hot, the Munde is solid. It malls partially in its uppermost region and only under special conditions. That's why volcanoes occur only in certain regions (you never have to worry about a volcano popping up in Miami!). The layer where the Munde malls partially and has small pockets of magma is the _________. 13. In the graph, this layer corresponds to number _____.

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Solution
Homework
11 months ago
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