Earth Science: The Physical Setting
Earth Science: The Physical Setting
1st Edition
Jeffrey C. Callister
ISBN: 9780133200409
Textbook solutions

All Solutions

Page 32: Practice Questions

Exercise 1
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1
Exercise 2
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minerals that form from magma form as the result of crystallization,evaporation,precipitation,condensation.
Exercise 3
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3
Exercise 4
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3
Exercise 5
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4
Exercise 6
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1
Exercise 7
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4
Exercise 8
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3
Exercise 9
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4
Exercise 10
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3
Exercise 11
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3
Exercise 12
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4
Exercise 13
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1
Exercise 14
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1
Exercise 15
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1
Exercise 16
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48° 32′ N
Exercise 17
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122° 03′ W
Exercise 18
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to East direction
Exercise 19
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2180 feet
Exercise 20
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4.25 mile
Exercise 21
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8 kilometers
Exercise 22
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1
Exercise 23
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Northeast direction
Exercise 24
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590 meters elevation.
Exercise 25
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Below is the topographic map of Cottonwood, Colorado.
![‘slader’](https://slader-solution-uploads.s3.amazonaws.com/6bf9ca5a-a7f1-4897-b331-32011d409016-1624622317781046.png)
Step 2
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To draw a profile of the topography along line AB in the map above, align first the transect line AB on the given grid marked with A and B.
![‘slader’](https://slader-solution-uploads.s3.amazonaws.com/9d4e7468-add8-4cd1-8686-3b3be8771556-1624622337239377.png)
Step 3
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Mark the intersection of the contour lines on the x-axis of the grid, and label the elevation of the contour lines.
![‘slader’](https://slader-solution-uploads.s3.amazonaws.com/b7227097-45bb-4de8-a116-21c5c303605b-1624612648313483.png)
Step 4
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Mark the contour line according to its elevation reflected in the y-axis.
![‘slader’](https://slader-solution-uploads.s3.amazonaws.com/e7a28ab0-242a-49de-957d-6aeeb122bd5f-1624612712973335.png)
Step 5
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Trace the points to make a topographic profile of the Cottonwood Creek.
![‘slader’](https://slader-solution-uploads.s3.amazonaws.com/7b08b412-12d0-4cfd-9468-7ff498af5f78-1624612477563995.png)
Exercise 26
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$a): gradiant = dfrac{change: in: field :value}{change: in :distance}$

$b):gradiant = dfrac{580-480}{2}$

$$
c)gradiant = dfrac{100}{2}=50 :m/km
$$

Exercise 27
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1
Exercise 28
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1
Exercise 29
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The map below is the given weather map which shows partial weather station data for several cities in eastern North America.
![‘slader’](https://slader-solution-uploads.s3.amazonaws.com/de3ade22-3256-4c1d-86b6-9fa067bdd099-1624624212039673.png)
Step 2
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Isotherm lines are drawn at a 10$^circ$ intervals. Temperatures lower than the isotherm value are always on one side of the isotherm and
higher temperatures are consistently on the other side. ![‘slader’]![‘slader’](https://slader-solution-uploads.s3.amazonaws.com/72e2576c-cd79-423b-9eb1-7ff597b23334-1624624217093523.png)
Exercise 30
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The map generated from problem 29 is shown below. The needed data from the map are the following:
$$ begin{aligned}
text{Richmond, Virginia temperature}&= 50^circ text{F} \
text{Hatteras, North Carolina temperature} &= 60^circ text{F}\
text{Distance between Richmond and Hatteras} &= 200 text{ miles}
end{aligned} $$

![‘slader’](https://slader-solution-uploads.s3.amazonaws.com/653b4bfa-3fa9-4d1e-9d81-1e76cc32dfed-1624624135904546.png)

Step 2
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(a) The equation for gradient is given by:
$$ begin{aligned}
text{gradient} &=frac{text{change in (amount of) field value}}{text{change in distance (horizontal distance}}\
end{aligned} $$
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(b) Plug known values in the equation in (a):
$$ begin{aligned}
text{gradient} &=frac{60^circ text{F}-50^circ text{F} }{200 text{ miles}}\
end{aligned} $$
Step 4
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(c) The average gradient is given by:
$$ begin{aligned}
text{gradient} &=frac{60^circ text{F}-50^circ text{F} }{200 text{ miles}}\
&=frac{10^circ text{F} }{200 text{ miles}} \
&=boxed{textbf{$0.05 dfrac{^circ text{F}}{text{mile}}$}}
end{aligned} $$
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$0.05 ^circ text{F per mile}$
Exercise 31
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Gradients can be estimated by observing how close the isolines between each other. If two isolines are closer together on a field map, the greater the gradient. And if two isolines are farther, the smaller the gradient.
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Based on the isolines in the map below, the city which is farthest from the isolines is New Orleans.
![‘slader’](https://slader-solution-uploads.s3.amazonaws.com/54aa1b95-d681-4821-b884-7b2514c9f6ea-1624625566833119.png)
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New Orleans
Exercise 32
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As illustrated in the map, temperatures generally decrease as latitude increases.
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Temperatures decrease as latitude increases.
Exercise 33
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Because it is representing something . so, it is considered a model.
Exercise 34
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oxygen and hydrogen.
Exercise 35
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the location will be between the lithosphere and atmosphere.
Exercise 36
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In the core of Glick planet
Exercise 37
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Latitude is 37° S
Exercise 38
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constant altitude, there will be no change because you are travelling through the same latitude.
Exercise 39
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Due to contour lines that are further apart indicates a slope that is relatively flat. and this area is wide which located between two far contour lines
Exercise 40
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a) NE direction.

b) Contour lines bend upstream.

Exercise 41
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The given topographic map below shows a location where a series of students went camping using mountain bicycles on July 1, 2003.
![‘slader’](https://slader-solution-uploads.s3.amazonaws.com/38d26484-ee0d-4288-9040-069d85d435d1-1624630312457279.png)
Step 2
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On July 2, 2003, they moved their campsite 1 mile directly east of their original campsite. The map below shows a plot of the new campsite established by the students.
![‘slader’](https://slader-solution-uploads.s3.amazonaws.com/69045975-8f30-4f71-b9bf-1d87bc32cf68-1624630318060036.png)
Exercise 42
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The map below shows the location of the campsite on July 2.
![‘slader’](https://slader-solution-uploads.s3.amazonaws.com/a5d1e174-bbb0-4381-bcc3-9a62724cd77d-1624630147839906.png)
Step 2
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We will draw the route in along the same elevation, and between two contour lines that are far apart so that they will travel in the least change in elevation. The map below shows the route from the new campsite to point P with the least change in elevation.
![‘slader’](https://slader-solution-uploads.s3.amazonaws.com/580ef292-1d39-4820-a973-7ce408ded2b2-1624630432959540.png)
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