Showing posts with label Physical Geology. Show all posts
Showing posts with label Physical Geology. Show all posts

Chapter 2. Origin of Earth & the Solar System - Review Questions

1. How can astronomers view events that happened in the universe’s distant past? 

2. In the image of three spectra at right, one is from the sun, and the other two are from galaxies. One of the galaxies is the Andromeda galaxy. Which spectrum is from Andromeda? 
Spectra for the sun and two galaxies. Source: Karla Panchuk (2015) CC BY 4.0.

3. Astronomers looking for some of the earliest stars in the universe were surprised to find a planetary system called HIP 11952, which existed 12.8 billion years ago. This was very early in the universe’s history, when stars still consisted largely of hydrogen and helium. Do you think there were terrestrial planets in this system? Why or why not? 

4. Summarize the trends in size and composition of objects in the solar system. 

5. What is the frost line, and what does it help to explain? 6. Why is Pluto not considered a planet? 

7. What is differentiation? 

8. The exoplanet Kepler-452b is within the habitable zone of its star. In our solar system, planets a similar distance from the Sun are terrestrial planets. Why can we not say for certain that Kepler-452b’s distance from its star means it is a terrestrial planet?

Answers to Review Questions 

1. To see an event, light from that event must reach our eyes. Light travels very quickly (about 300,000,000 m/s), but the universe is very, very large. Depending on how far away the event was, it could take billions of years for light to travel from the event to our eyes so we can see it. Astronomers take advantage of this fact to view the universe’s past. 

2. B is the spectrum from the Andromeda galaxy. We know that one spectrum represents the sun, which is not moving toward or away from us. (Our orbit is not perfectly circular, but the small eccentricity is not a factor in this comparison.) We know that the Andromeda galaxy is on a collision course with us, so it is the exception to the rule that galaxies are moving away from us, and their light is red-shifted. That means the spectrum B which is shifted furthest to the left (blue-shifted) is Andromeda, and spectrum A which is furthest to the right (red-shifted) is a galaxy moving away from us. That means C is the sun. 

3. The planetary system consisted of two Jupiter-sized gas giant planets. Gas giant planets contain large amounts of hydrogen, and hydrogen was plentiful in the early universe. In contrast, terrestrial planets have heavier elements, especially silica, iron, magnesium, and nickel, that had yet to be manufactured by stars. Those elements were not present in sufficient abundance to form terrestrial planets until much later. 

4. Closest to the sun we find the small, rocky, terrestrial planets with metal cores. Further out are the gas giant planets, which are the largest in the solar system. They consist mostly of hydrogen, and have cores of rock and ice. Beyond the gas giant planets are the ice giant planets, which are next largest. They have a mantle of ice (not just water ice but ammonia and methane ice), and a rocky core. Smaller objects in the solar system include rocky bodies within the asteroid belt between Mars and Jupiter, and bodies of ice and dust in the Kuiper belt and Oort cloud beyond Neptune.

5. The frost line marks the distance from the sun beyond which temperatures were cool enough to allow ice to form. This helps to explain why the terrestrial planets are closer to the sun, and the Jovian and ice giant planets farther away. Mineral grains could solidify and begin to accrete closer to the sun, forming terrestrial planets, because they have higher melting points. In contrast, water vapour, methane, and ammonia had to be farther from the sun before they could freeze and begin to accrete. 

6. Planets are defined as having cleared their orbits of debris. Pluto is located within the Kuiper belt, so it shares its orbit with other objects. There are two other criteria in the definition of a planet: planets in our solar system must orbit the sun, and they must have a spherical shape. Pluto satisfies both these criteria, but sadly the people deciding whether or not Pluto should be a planet are not amenable to a “best two out of three” compromise. 

7. Differentiation is the separation of materials within a planet such that dense materials sink to the core. In Earth’s case, the denser materials are iron and nickel. 

8. The fact that we have terrestrial planets close to the sun makes sense in terms of the frost line, but it does not seem to be a hard-and-fast rule in other planetary systems. Therefore, we can’t conclude from Kepler452b’s position alone that it is a terrestrial planet. 

9. The rules of the accretion game mean that there are many complex interactions, so even a small difference in the starting conditions or in how the game goes in the beginning could have major implications in the end. For that reason, we shouldn’t expect to find a planetary system that matches ours in every minute detail. However, just because we haven’t found a similar planetary system does not mean one does not exist. Our planet-finding methods are biased toward discovering large planets orbiting close to their stars, whereas our solar system has small planets close to the sun and larger ones farther away. That doesn’t mean our methods won’t eventually turn up a system like ours, just that they are more likely to turn up systems that are different.

Chapter 6. The Rock Cycle - Review Questions

Review Questions 
1. What processes must take place to transform rocks into sediment? 
2. What processes normally take place in the transformation of sediments to sedimentary rock
3. What are the processes that lead to the formation of a metamorphic rock?


Answers to Review Questions
1. The rock must be exposed at surface. This means uplift and removal of overlying rocks and sediments is required. Once exposed, chemical and/or physical weathering can reduce the rock to smaller loose fragments (sediments). The sediments can be eroded and then transported by a variety of mechanisms. 

2. Sediments are buried beneath other sediments, where pressure compacts the sediments, forcing grains closer together. Mineral cement forms around the grains, binding them to each other and into solid rock. 

3. Rock is buried deeply in the crust and exposed to very high temperatures and pressures. Under those conditions, a new type of rock is formed when minerals undergo physical changes and chemical reactions.

Question - Explain the difference between porphyritic and pegmatitic textures.

Explain the difference between porphyritic and pegmatitic textures.

ANSWER:
In porphyritic rocks there are two distinct crystal sizes that are indicative of two stages of cooling (slow then fast). The fine material can range from glass to several mm, as long as the coarse crystals are distinctively larger. In pegmatitic rocks the crystals are consistently coarser than 1 cm, and can be much larger. Pegmatites form the slow cooling of water-rich magmas. 

Question - What processes normally take place in the transformation of sediments to sedimentary rock?

What processes normally take place in the transformation of sediments to sedimentary rock?

ANSWER:
Sediments are buried beneath other sediments where, because of the increased pressure, they become compacted and dewatered. With additional burial they are warmed to the point where cementing minerals can form between the grains (less than 200˚C).

Question - What processes must take place to transform rocks into sediment?

What processes must take place to transform rocks into sediment?

ANSWER:
The rock must be exposed at surface so in many cases uplift and removal of overlying sedi‐ ments is required. Then chemical and/or physical weathering can take place, which reduces the rock to smaller loose fragments. These fragments are sediments that can be eroded and then transported by a variety of maechanisms. 

Question - Explain how the need for an atom’s outer shell to be filled with electrons contributes to bonding.

Explain how the need for an atom’s outer shell to be filled with electrons contributes to bonding.

ANSWER:
The element’s atomic number will determine the extent to which its outer layers are popu‐ lated with electrons. If the outer shell is not quite full, the atom may gain electrons to fill them and become an anion (negative charge). If the outer shell has only a few electrons, it may lose them and become a cation (positive charge). Cations and anions attract each other to form mol‐ ecules with ionic bonding.

Question - What allows magnesium to substitute freely for iron in olivine?

What allows magnesium to substitute freely for iron in olivine?

ANSWER:
Magnesium can substitute freely for iron in olivine and several other minerals because they have similar charges (+2) and similar ionic radii.

Question - How are the silica tetrahedra structured differently in pyroxene and amphibole?

How are the silica tetrahedra structured differently in pyroxene and amphibole?

ANSWER:
Pyroxene is made up of single chains of tetrahedra while amphibole is made up of double chains.

Question - Why is biotite called a ferromagnesian mineral, while muscovite is not?

Why is biotite called a ferromagnesian mineral, while muscovite is not?

ANSWER:
Biotite includes iron and/or magnesium in its formula, while muscovite does not.

Question - You have an unknown mineral that can scratch glass but cannot scratch a porcelain streak plate. What is its approximate hardness?

You have an unknown mineral that can scratch glass but cannot scratch a porcelain streak plate. What is its approximate hardness?

ANSWER:
Glass has a Mohs hardness of about 5.5 while porcelain is close to 6.5. The mineral is be‐ tween these two, so it must be close to 6.

Question - In what way is a mineral different from a rock?

In what way is a mineral different from a rock?

ANSWER:
A mineral has a specific chemical composition and lattice structure. Rocks are made out of minerals, and most rocks contain several different types of minerals. 

Question - What is the main component of Earth’s core?

What is the main component of Earth’s core?

ANSWER:
The main component of Earth’s core is iron (Fe).

Question - What process leads to convection in the mantle?

What process leads to convection in the mantle?

ANSWER:
Transfer of heat from the core to the mantle leads to heating of lower mantle rock. When heated, the rock expands and its density is reduced. Because the mantle is plastic, this lowerdensity material tends to rise toward the surface, and cooler denser mantle material moves in to take its place.

Question - How does mantle convection contribute to plate tectonics?

How does mantle convection contribute to plate tectonics?

ANSWER:
Mantle convection creates the traction that can force plates to move around on the surface.

Question - What are some of the processes that take place at a divergent plate boundary?

What are some of the processes that take place at a divergent plate boundary?

ANSWER:
Hot mantle rock moving toward the surface partially melts because the pressure is reduced. The magma produced moves upward into cracks in the crust and is extruded onto the sea floor.

Question - Dinosaurs first appear in the geological record in rocks from about 215 Ma and then became extinct 65 Ma.

Dinosaurs first appear in the geological record in rocks from about 215 Ma and then became extinct 65 Ma. For what proportion (%) of geological time did dinosaurs exist?

ANSWER:
215 – 65 = 150 Ma. Since the age of the Earth is 4570 Ma, this represents 150/4,570 = 0.033 or 3.3% of geological time.

Question - Describe the lattice structure and elemental composition of the mineral halite.

Describe the lattice structure and elemental composition of the mineral halite.

Answer:
Halite is composed of sodium (Na) and chlorine (Cl) with the Na+ and Cl- ions alternating with one another in all three directions within a cubic structure.

Question - List three ways in which geologists can contribute to society.

List three ways in which geologists can contribute to society.

Answer:
Geologists provide information to reduce the risk of harm from hazards such as earthquakes, volcanoes, and slope failures; they play a critical role in the discovery of important resources; they contribute to our understanding of life and its evolution through paleontological studies; and they play a leading role in the investigation of climate change, past and present and its implications.

Question - How would some familiarity with biology be helpful to a geologist?

How would some familiarity with biology be helpful to a geologist?

Answer:
Paleontology is an important aspect of geology and requires an understanding of biology, including evolution, the physiology of animals and plants and ecological relationships.

Question - In what way is geology different from the other sciences, such as chemistry and physics?

  • In what way is geology different from the other sciences, such as chemistry and physics?

Answer:
Geology involves integration of various different sciences (chemistry, physics, and biology for example), but also requires an understanding of the importance of billions of years of geological time.

Search This Blog