Physical Science
10th Edition
ISBN: 9780073513898
Author: Bill Tillery
Publisher: MCGRAW-HILL HIGHER EDUCATION
expand_more
expand_more
format_list_bulleted
Concept explainers
Textbook Question
Chapter 18, Problem 48AC
Which type of plate boundary accounts for the formation of the Appalachian Mountains?
a. Divergent
b. Ocean to continental convergence
c. Continental to continental convergence
d. Transform
Expert Solution & Answer
Want to see the full answer?
Check out a sample textbook solutionStudents have asked these similar questions
Which of the following is most responsible for the
formation of new crust ar the edge of a tectonic
plate?
A. mountain building at a continent-continent
convergent boundary
B. magma rising up from the mantle at a
divergent boundary
С.
two tectonic plates sliding past one another at
a transform boundary
D.
subduction of one oceanic plate under another
at a convergent boundary
11. Which part of the Earth is a hot, elastic semi-liquid layer that extends around the entire Earth?A. crust
B. core
C. mantle
D. asthenosphere
If we pushed the Earth closer to the Sun, it would develop a thick, CO2-rich atmosphere like Venus. All of that CO2 would come from the Earth's
a.
sea floor after the oceans evaporate
b.
mantle after the crust melts
c.
volcanic eruptions which would become more frequent
d.
polar regions after the ice caps melt
Chapter 18 Solutions
Physical Science
Ch. 18 - 1. The core of Earth is composed of
a. iron and...Ch. 18 - 2. The middle part of Earth's interior is
a....Ch. 18 - 3. The separation of materials that gave Earth its...Ch. 18 - 4. A vibration that moves through any part of...Ch. 18 - 5. The S-wave is a
a. longitudinal wave.
b....Ch. 18 - 6. Waves that occur where S- or P-waves reach the...Ch. 18 - 7. The three main areas of Earth’s interior are
a....Ch. 18 - 8. The boundary between the crust and the mantle...Ch. 18 - 9. The mantle is composed of
a. sulfides.
b....Ch. 18 - 10. Seismological studies suggests that the...
Ch. 18 - 11. Evidence from meteorite studies proposes that...Ch. 18 - 12. The layer in Earth where seismic waves sharply...Ch. 18 - 13. The layer that is broken up into plates that...Ch. 18 - 14. The name of the single large continent...Ch. 18 - 15. Records of the strength and directions of...Ch. 18 - 16. The chain of mountains found in the center of...Ch. 18 - 17. Long, deep, and narrow oceanic trenches are...Ch. 18 - 18. The theory that the lithosphere is composed of...Ch. 18 - 19. The plate boundary associated with the...Ch. 18 - 20. The movement of one plate under another plate...Ch. 18 - 21. Transform boundaries occur when
a. two plates...Ch. 18 - 22. What is the current theory about why the...Ch. 18 - 23. The seismic waves that cause the most damage...Ch. 18 - 24. Earth’s mantle has a chemical composition that...Ch. 18 - 25. From seismological data, Earth’s shadow zone...Ch. 18 - 26. The Mohorovicic discontinuity is a change in...Ch. 18 - 27. The oldest rocks are found in
a. continental...Ch. 18 - 28. The least dense rocks are found in
a....Ch. 18 - 29. The idea of seafloor spreading along the...Ch. 18 - 30. According to the plate tectonics theory,...Ch. 18 - 31. The presence of an oceanic trench, a chain of...Ch. 18 - 32. The presence of an oceanic trench with shallow...Ch. 18 - 33. The ongoing occurrence of earthquakes without...Ch. 18 - 34. The evidence that Earth's core is part liquid...Ch. 18 - 35. The surfaces of early planets in our solar...Ch. 18 - 36. The early Earth’s core is thought to have...Ch. 18 - 37. Indirect evidence that supports the theory of...Ch. 18 - 38. The oceanic crust is
a. thicker than the...Ch. 18 - 39. Seismic waves that do not travel through...Ch. 18 - 40. The fastest seismic wave is the
a. P-wave.
b....Ch. 18 - 41. Information about the composition and nature...Ch. 18 - 42. Primary information about the nature of the...Ch. 18 - 43. The asthenosphere is not defined as
a....Ch. 18 - 44. Earth’s magnetic field is thought to be...Ch. 18 - 45. Studies of the Mid-Atlantic Ridge provided...Ch. 18 - 46. Evidence that supports seafloor spreading does...Ch. 18 - 47. A geologic feature that was produced by...Ch. 18 - 48. Which type of plate boundary accounts for the...Ch. 18 - 49. Which type of plate boundary was responsible...Ch. 18 - 50. A famous transform boundary in the United...Ch. 18 - 51. Plate movement is measured by
a. reflected...Ch. 18 - 52. Islands that form when melted subducted...Ch. 18 - 1. Describe one theory of how Earth came to have a...Ch. 18 - 2. Briefly describe the internal composition and...Ch. 18 - 3. What is the asthenosphere? Why is it important...Ch. 18 - 4. Describe the parts of Earth included in the (a)...Ch. 18 - 5. What is continental drift? How is it different...Ch. 18 - 6. Rocks, sediments, and fossils around an oceanic...Ch. 18 - 7. Describe the origin of the magnetic strip...Ch. 18 - 8. Explain why ancient rocks are not found on the...Ch. 18 - 9. Describe the three major types of plate...Ch. 18 - 10. What is an island arc? Where are they found?...Ch. 18 -
11. Briefly describe a model that explains how...Ch. 18 - 12. Briefly describe the theory of plate tectonics...Ch. 18 - 13. What is an oceanic trench? What is the...Ch. 18 - 14. Describe the probable source of all the...Ch. 18 - 15. The northwestern coast of the United States...Ch. 18 - 16. Explain how the crust of Earth is involved in...Ch. 18 - 1. Why are there no active volcanoes in the...Ch. 18 - 2. Describe cycles that occur on Earth's surface...Ch. 18 - 3. Discuss evidence that would explain why plate...Ch. 18 - 4. Analyze why you would expect most earthquakes...Ch. 18 - 1. The rate at which the temperature increases...Ch. 18 - 2. Based on a geothermal gradient of 15°C/km, what...Ch. 18 - 3. Based on a geothermal gradient of 250C/km, what...Ch. 18 - 4. What is the pressure, in N/m2, at the depth of...Ch. 18 - 5. What is the pressure, in N/m2, at a depth of 75...Ch. 18 - 6. What is the pressure, in N/m2, at the base of...Ch. 18 - 7. Wood floating in water can demonstrate how the...Ch. 18 - 8. A teacher would like to demonstrate the...Ch. 18 - 9. A survey of a mid-oceanic ridge determined the...Ch. 18 - 10. GPS stations on two separate plates have...Ch. 18 - 11. What is the geothermal gradient along a...Ch. 18 - 12. What are the subduction direction and slope of...Ch. 18 - 13. What are the subduction direction and slope,...Ch. 18 - 14. Earthquake data from a subduction zone are...Ch. 18 - 15. The North American Plate is moving west at a...
Additional Science Textbook Solutions
Find more solutions based on key concepts
The formula for the sum Sn of the geometric series Sn=a+ar+.....arn−1 .
Mathematical Methods in the Physical Sciences
Explain what happens to the energy carried by light that it is dimmed by passing it through two crossed polariz...
College Physics
8. The formula ΔU = nCvΔT for the change in the internal energy of a fixed amount of an ideal gas is valid
only...
College Physics (10th Edition)
Separate the list P,F,V,,T,a,m,L,t, and V into intensive properties, extensive properties, and nonproperties.
EBK FUNDAMENTALS OF THERMODYNAMICS, ENH
Why is physics the most basic science?
Conceptual Physics: The High School Physics Program
Choose the best answer to each of the following. Explain your reasoning. Which of these star clusters is oldest...
Cosmic Perspective Fundamentals
Knowledge Booster
Learn more about
Need a deep-dive on the concept behind this application? Look no further. Learn more about this topic, physics and related others by exploring similar questions and additional content below.Similar questions
- Review. The North American and European plates of the Earths crust are drifting apart with a relative speed of about 25 mm/yr. Take the speed as constant and find when the rift between them started to open, to reach a current width of 2.9 103 mi.arrow_forward5. The "iceberg analogy" for the isostatic equilibrium of the continental crust turns out to be quite the relative density of icebergs versus seawater is close to the relative density of continental crust versus mantle. Glacial ice is about 15% less dense than seawater; likewise continental crust is about 15% less dense than the mantle. This leads to a simple rule that we can call the 1-to-8 rule: for every 1 unit of extra elevation for an iceberg or a mountain belt, there need to be 8 units of total thickness. These iceberg examples illustrate the idea: an iceberg 3 meters above sea level is 24 meters thick an iceberg 1 meter above sea level is 8 meters thick an iceberg 2 meters above sea level is 16 meters thick 3m 2m water level 1m >7m 14m 21m For the following questions, apply the 1-to-8 rule, assuming continental crust in isostatic equilibrium. a. Continental crust at sea level averages about 35 kilometers thick. (1 km = 0.6 miles.) Therefore, in general, how thick must the crust…arrow_forward13. How deep in the crust is 10 kbar? Lithostatic pressure within the crusts results from the weight of the rocks above. Assume an average density of 2750 kg/m3. Use the equation P=p*g*h or P/(p *g)=h 23kPa/m P=pressure (e.g. kbar), p=density, g-gravity 9.8 m/s2, h= depth (m), 1 kbar=1,000 bars, 1 bar=100,000 Pa, 1 Pa=kg/(m*s2), 1 kbar =100,000,000 Pa, 1 km =1000 m. Give your answer in kilometers.arrow_forward
- 7. The P-wave from an earthquake arrives at a seismo- graph station at 10:20 a.m. and the S-wave arrives atarrow_forwardFrom Hawaii to the bend in the Hawaiian-Emperor chain is about 4000 km. Use the speed of Pacific plate motion given in Problem 7 to estimate how long ago the direction of plate motion changed. (Note: It may not be a coincidence that the San Andreas fault became active in what is now Southern California at about the same time.) 7. The Hawaiian-Emperor chain of undersea volcanoes is about 7500 km long, and the Pacific plate is moving 9.2 cm a year. How old is the oldest detectable volcano in the chain? What has happened to older volcanoes in the chain?arrow_forward1. A giant ice sheet expands quickly over the surface of North America. For how long must the ice sheet remain in place in order to cool the crust to a depth of 2000 m? The thermal diffusivity of crustal rocks is ~ 10-6 m²/s. Give your answer in years.arrow_forward
- b. Under what condition is a material or a rock mass considered to: i. Have positive Poisson’s ratio ii. Have negative Poisson’s ratio iii. Possess planar discontinuity iv. Exhibit positive deformation v. Exhibit negative deformation?arrow_forward4. Assuming there are no major changes in either the discharge of the river or the slope of the channel, which image shows the most likely course of the river in 500 years? Original river %3 A O A. Image A O B. Image B OC. Image C D. There is no way to determine which image is most likelyarrow_forward3. Prove that the slope of the internal fault characteristics for a single-end-fed system is 200%. Varrow_forward
- Q2. To illustrate the tremendous pressure that exists deep underground where granite bodies are emplaced, answer the following question. Stone Mountain granite in Georgia has an area of 4.1 square kilometers and was emplaced 16 km deep. If we assume that Stone Mountain granite is present in an area that has more or less a rectangular shape with dimensions of 1 km by 4.1 km and that it was buried under 16 km of metamorphic rock material with a density of 2.6 g/cm³. We can calculate the weight of metamorphic rock over the Stone Mountain granite when it was emplaced and before erosion removed that material. First, we need the volume of the metamorphic rock that existed over Stone Mountain. The volume of a rectangular prism that represents the metamorphic rock over Stone Mountain is length x width x height. In our case: 1 km x 4.1 km x 16 km= 65.6 km³ Now we can use the relationship: Density x Volume= Mass However, we need to change our density units from 2.6 g/cm3 to kg/km3, and then we…arrow_forwardA seismic survey is conducted in a region with two layers. The top layer is shale, with density 2500 kg/m3, and seismic velocity of 2900m/s, and the bottom layer is sandstone, with a density of 2100 kg/m3, and a seismic velocity of 3000m/s. The reflection coefficient will bea. Positiveb. Negativec. Zerod. Not enough informationarrow_forwardThe ocean is mostly heated from the top, by light from the sun. The warmer surface water doesn’t mix much with the colder deep ocean water. This lack of mixing can be ascribed to a lack ofA. Conduction. B. Convection.C. Radiation. D. Evaporation.arrow_forward
arrow_back_ios
SEE MORE QUESTIONS
arrow_forward_ios
Recommended textbooks for you
- An Introduction to Physical SciencePhysicsISBN:9781305079137Author:James Shipman, Jerry D. Wilson, Charles A. Higgins, Omar TorresPublisher:Cengage LearningAstronomyPhysicsISBN:9781938168284Author:Andrew Fraknoi; David Morrison; Sidney C. WolffPublisher:OpenStax
- Horizons: Exploring the Universe (MindTap Course ...PhysicsISBN:9781305960961Author:Michael A. Seeds, Dana BackmanPublisher:Cengage LearningFoundations of Astronomy (MindTap Course List)PhysicsISBN:9781337399920Author:Michael A. Seeds, Dana BackmanPublisher:Cengage LearningPhysics for Scientists and Engineers, Technology ...PhysicsISBN:9781305116399Author:Raymond A. Serway, John W. JewettPublisher:Cengage Learning
An Introduction to Physical Science
Physics
ISBN:9781305079137
Author:James Shipman, Jerry D. Wilson, Charles A. Higgins, Omar Torres
Publisher:Cengage Learning
Astronomy
Physics
ISBN:9781938168284
Author:Andrew Fraknoi; David Morrison; Sidney C. Wolff
Publisher:OpenStax
Horizons: Exploring the Universe (MindTap Course ...
Physics
ISBN:9781305960961
Author:Michael A. Seeds, Dana Backman
Publisher:Cengage Learning
Foundations of Astronomy (MindTap Course List)
Physics
ISBN:9781337399920
Author:Michael A. Seeds, Dana Backman
Publisher:Cengage Learning
Physics for Scientists and Engineers, Technology ...
Physics
ISBN:9781305116399
Author:Raymond A. Serway, John W. Jewett
Publisher:Cengage Learning
A Level Physics – Ideal Gas Equation; Author: Atomi;https://www.youtube.com/watch?v=k0EFrmah7h0;License: Standard YouTube License, CC-BY