Geology Lab Test 1 Quiz - Plate Tectonics Q & A
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Geology Lab Test 1 Quiz - Plate Tectonics Q & A
1.
Which of the following correctly lists the main zones of the Earth's interior, along with their compositions
and phases?
A) 1. Outer Core (solid phase; Fe-Mg-rich), 2. Crust (liquid phase; Si-Al-rich), 3. Inner Core (solid phase; Fe-Ni-rich), 4. Mantle (solid phase; Fe-Mg-rich, plastic flow)
B) 1. Mantle (solid phase; Fe-Mg rich, plastic flow), 2. Inner Core (liquid phase; Fe-Ni-rich), 3. Crust (solid phase; Si-Al-rich continental and Fe-Mg-rich oceanic varieties), 4. Outer Core (solid phase; Fe-
Ni-rich)
C) 1. Crust (solid phase; Si-Al-rich continental and Fe-Mg-rich oceanic varieties), 2. Mantle (solid phase; Fe-Mg rich, plastic flow), 3. Outer Core (liquid phase; Fe-Ni-rich), 4. Inner Core (solid phase; Fe-
Ni-rich)
D) 1. Outer Core (liquid phase; Fe-Ni-rich), 2. Inner Core (solid phase; Fe-Ni-rich), 3. Mantle (solid phase; Fe-Mg rich, plastic flow), 4. Crust (solid phase; Si-Al-rich continental and Fe-Mg-rich oceanic varieties)
Answer: C) 1. Crust (solid phase; Si-Al-rich continental and Fe-Mg-rich oceanic varieties), 2. Mantle (solid phase; Fe-Mg rich, plastic flow), 3. Outer Core (liquid phase; Fe-Ni-rich), 4. Inner Core (solid phase; Fe-Ni-
rich). This option correctly lists the main zones of the Earth's interior in their respective order, along with their compositions and phases.
2.
How might the internal heterogeneity of the Earth influence what happens on the surface?
A) Variations in mantle composition affect the flow of magma and the location of volcanic activity.
B) Differences in core temperature impact the rotation speed of the Earth.
C) Variations in the inner core density affect the strength of the Earth's magnetic field.
D) Variations in crustal thickness determine the intensity of earthquakes.
Answer: A) Variations in mantle composition affect the flow of magma and the location of volcanic activity.
Explanation: The internal heterogeneity of the Earth, particularly variations in composition and temperature within the mantle, can significantly influence surface phenomena. Variations in mantle composition affect the flow of magma, which in turn impacts the location, frequency, and intensity of volcanic activity. For example, regions with hotter mantle material may experience more vigorous magma upwelling, leading to increased volcanic activity, while cooler regions may have less frequent eruptions. Therefore, understanding the internal structure and composition of the Earth is crucial for predicting and managing volcanic hazards on the surface.
3.
What are the lithosphere and asthenosphere?
A) The lithosphere is the rigid outer layer of the Earth composed of the crust and upper mantle, while the asthenosphere is a partially molten, ductile layer beneath the lithosphere.
B) The lithosphere is a partially molten layer beneath the Earth's crust, while the asthenosphere is the rigid outer layer composed of solid rock.
C) The lithosphere is the region of the Earth's mantle where convection currents occur, while the asthenosphere is the solid layer above the Earth's core.
D) The lithosphere is the outermost layer of the Earth's core, while the asthenosphere is a layer of dense rock located between the lithosphere and the mantle.
Answer: A) The lithosphere is the rigid outer layer of the Earth composed of the crust and upper mantle, while the asthenosphere is a partially molten, ductile layer beneath the lithosphere.
Explanation: The lithosphere refers to the rigid outer layer of the Earth, including the crust and the uppermost part of the mantle. It is relatively cool and rigid, behaving as a brittle solid. In contrast, the asthenosphere lies
beneath the lithosphere and consists of partially molten, ductile rock. It exhibits plastic behavior and allows for the slow flow of solid material over geological timescales. This distinction between the lithosphere and asthenosphere is crucial for understanding the behavior of tectonic plates and the movement of the Earth's surface.
4.
In 1912, Alfred Wegener proposed the hypothesis of "continental drift" to explain the formation of landmasses and oceans. What evidence supported Wegener's hypothesis?
A) Wegener's hypothesis was supported by evidence of similar climates across different continents.
B) The hypothesis was based on the discovery of fossilized dinosaur remains found on separate continents.
C) Evidence such as conformable coastlines, similar fossil assemblages, and rock types from continent to continent supported Wegener's hypothesis.
D) Wegener's hypothesis was primarily based on the observation of matching mountain ranges on different continents.
Answer: C) Evidence such as conformable coastlines, similar fossil assemblages, and rock types from continent to continent supported Wegener's hypothesis.
Explanation: Alfred Wegener's hypothesis of continental drift was supported by various lines of evidence, including conformable coastlines (e.g., the fit of the coastlines of Africa and South America), similar fossil assemblages found on separate continents (e.g., the presence of identical fossils of plants and animals), and matching rock types and geological features across different continents. These observations suggested that the continents were once connected and had drifted apart over geological time scales, supporting Wegener's proposal of continental drift.
4. How did paleomagnetic studies contribute to understanding the Earth's magnetic field?
A) Paleomagnetic studies revealed that the Earth's magnetic field is generated by the movement of tectonic plates.
B) Paleomagnetic studies demonstrated that the Earth's magnetic field is primarily caused by the rotation of the inner core.
C) Paleomagnetic studies provided evidence that the Earth's magnetic field is generated by convection in the outer core.
D) Paleomagnetic studies showed that the Earth's magnetic field is solely influenced by the alignment of magnetic minerals in the crust.
Answer: C) Paleomagnetic studies provided evidence that the Earth's magnetic field is generated by convection in the outer core.
Explanation: Paleomagnetic studies involve analyzing the magnetic properties of rocks to understand the Earth's magnetic field in the past. By examining the alignment of magnetic minerals in ancient rocks, researchers can determine the orientation of the Earth's magnetic field at the time of the rocks' formation. Through these studies, scientists have found evidence supporting the hypothesis that the Earth's magnetic field is generated by convection currents in the outer core, where molten iron and nickel create electric currents
that generate the magnetic field. Therefore, option C is the correct answer as it accurately reflects the contribution of paleomagnetic studies to understanding the Earth's magnetic field.
5.
Has the orientation of the Earth's magnetic field remained fixed over millions of years?
A) Yes, the orientation of the Earth's magnetic field has remained constant throughout geological history.
B) No, the orientation of the Earth's magnetic field has reversed several times over millions of years.
C) Yes, but the orientation of the Earth's magnetic field has shifted slightly due to changes in the Earth's rotation.
D) No, the orientation of the Earth's magnetic field is influenced by the alignment of magnetic minerals in the Earth's crust.
Answer: B) No, the orientation of the Earth's magnetic field has reversed several times over millions of years.
Explanation: The Earth's magnetic field has not remained fixed over geological time. Paleomagnetic studies have shown that the Earth's magnetic field has undergone numerous reversals, where the magnetic north and south poles switch places. These reversals, known as geomagnetic reversals, have occurred irregularly over millions of years. The cause of geomagnetic reversals is not fully understood, but they are believed to be related to changes in the Earth's outer core, such as convection currents. Therefore, option B is the correct answer as it reflects the dynamic nature of the Earth's magnetic field orientation over time.
6.
How did paleomagnetic studies contribute to understanding the Earth's magnetic field?
A) Paleomagnetic studies revealed that the Earth's magnetic field is generated by the movement of tectonic plates.
B) Paleomagnetic studies demonstrated that the Earth's magnetic field is primarily caused by the rotation of the inner core.
C) Paleomagnetic studies provided evidence that the Earth's magnetic field is generated by convection in the outer core.
D) Paleomagnetic studies showed that the Earth's magnetic field is solely influenced by the alignment of magnetic minerals in the crust.
Answer: C) Paleomagnetic studies provided evidence that the Earth's magnetic field is generated by convection in the outer core.
Explanation: Paleomagnetic studies involve analyzing the magnetic properties of rocks to understand the Earth's magnetic field in the past. By examining the alignment of magnetic minerals in ancient rocks, researchers can determine the orientation of the Earth's magnetic field at the time of the rocks' formation. Through these studies, scientists have found evidence supporting the hypothesis that the Earth's magnetic field is generated by convection currents in the outer core, where molten iron and nickel create electric currents
that generate the magnetic field. Therefore, option C is the correct answer as it accurately reflects the contribution of paleomagnetic studies to understanding the Earth's magnetic field.
7.
What is the Curie Point?
A) The temperature at which certain minerals gain magnetization.
B) The temperature at which certain minerals lose their magnetization.
C) The temperature at which the Earth's magnetic field reverses.
D) The temperature at which certain minerals align with the Earth's magnetic field.
Answer: B) The temperature at which certain minerals lose their magnetization.
Explanation: The Curie Point is the temperature at which certain minerals lose their magnetization due to the thermal energy of atoms becoming high enough to disrupt the alignment of their magnetic poles.
8.
What does orientation refer to in paleomagnetism?
A) The angle from the horizontal.
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