PHSC 210 WEEK 5 Mastering Geology Assignments | Assignment Help | Liberty University
- Liberty University / PHSC 210
- 08 Aug 2017
- Price: $15
- Other / Other
PHSC 210 WEEK 5 Mastering Geology Assignments
8
Mastering Geology
Assignments 8
Item 1
Part A
Which of the
following is the primary step that allows water to enter the groundwater
system?
o evaporation |
o infiltration |
o runoff |
o precipitation |
Part B
Which of the
following statements about the global water supply is true?
o Decreased
precipitation could affect water supply available for humans. |
o Most of the global
freshwater supply is easily accessible. |
o A majority of the
world’s water is drinkable by humans. |
o Rivers are the most
likely source of water for humans. |
o The loss of
glaciers and ice sheets due to climate change will not have a large impact of
global freshwater supply. |
Part C - Ranking water sources
Rank the
following sources of water from largest to smallest in terms of percentage of
the world’s total supply.
Rank from largest to smallest. To rank items as
equivalent, overlap them.
Item 2
Stream drainage
patterns develop in response to variability in the material over which the
streams are flowing and by following the path of least resistance. As they flow
downslope due to gravity, a number of factors can influence where streams will
establish their channels.
Some of these factors present variability in
resistance to erosion caused by differences in rock type, degree of fracturing,
and/or underlying geologic structures. Stream drainage patterns can often
provide clues about the geology underlying the landscape.
Drainage patterns:
·
Dendritic drainage patterns resemble a branching
tree. Dendritic patterns are the most common type of stream drainage, and
typically form where streams flow over materials that are uniform in their
resistance to erosion.
·
Radial drainage patterns develop where streams
radiate outward from an isolated high area.
·
Rectangular drainage patterns can form where
streams flow over rocks that are heavily fractured. Since fractures (joints)
often run nearly perpendicular to each other, stream channels in a rectangular
drainage pattern join each other at right angles as they follow the fractured,
more easily eroded bedrock.
·
Trellis drainage patterns form where streams
flow over alternating bands of harder and softer ground (for example, flowing
over folded layers of alternating resistant and less resistant rock). This
pattern of erodible and less erodible ground leads to channels that run nearly
parallel to one another, connected in breaks in ridgelines. These have the
appearance of a garden trellis.
Part A - Classifying stream
drainage patterns
Drag the appropriate labels to their respective
targets.
Part B - The origin of the stream
drainage patterns
Item 3
Part A
Which of the following rivers is the largest river in North America?
o the Mississippi
River |
o the Colorado River |
o the Missouri River |
o the Rio Grande |
o the Mackenzie River |
Part B
Which of the following choices does not directly affect stream velocity?
o stream gradient |
o stream discharge |
o channel shape |
o channel size |
o location of the
drainage divide |
Part C
The amount of meandering that occurs in a stream influences the gradient in which of the following ways?
o With more meanders,
the stream gradient increases. |
o Meanders do not
cause a change in stream gradient. |
o With more meanders,
the stream gradient decreases. |
o With more meanders,
the gradient will change, but only where the stream enters the ocean. |
o Having more
meanders increases the stream's potential for flooding. |
Part D
What type of drainage pattern would you expect to find developing on rocks that have been folded and exposed by differential erosion over time?
o a trellis drainage
pattern |
o a yazoo drainage
pattern |
o a rectangular
drainage pattern |
o a radial drainage
pattern |
o a dendritic
drainage pattern |
Part E
While working on a stream in your field study area, you find that the channel width is 20 meters, the channel depth is 2 meters, and the velocity is 1.2 meters/second. What is the discharge of this stream?
o 4.8 m3/s |
o 23.2 m3/s |
o 48 m3/s |
o 10.6 m3/s |
o 480 m3/s |
Item 4
Streams reshape
the landscape through erosion and deposition of continental earth. Erosion
removes earth, which creates stream channels and stream valleys. Deposition, on
the other hand, allows sediment to accumulate in an area. The force of flowing
stream water determines whether erosion or deposition will occur at a
particular location along a stream. In order for a stream to move sediment, the
force of stream water flow must be greater than the frictional forces holding
the sediment grains in place. Recall that
force = mass × acceleration
Thus, we would expect erosion to occur where stream
water has high acceleration and deposition to occur where
stream water has low (even negative) acceleration.
Part A - Erosion and deposition
along a meandering stream
Part B
- Base level and stream valleys
Part C
- Stream features
A river system can be divided into three zones: a zone of
erosion, a zone of transportation, and a zone of
deposition, as shown in the figure below.
Determine the zone
where each of the depicted features occurs.
Drag the appropriate items into their respective
bins. Each item may be used only once.
Item 5
Part A
Which of the
following zones is the location of the most biological activity?
o the unsaturated
zone |
o the zone of soil
moisture |
o the zone of
saturation |
o the intermediate
belt |
o the capillary
fringe |
Part B
In terms of
freshwater storage, groundwater is second only to which of the following
sources?
o the atmosphere |
o soil moisture |
o freshwater lakes |
o stream channels |
o glaciers |
Part C
The majority of
groundwater is stored within which of the following zones?
o the zone of
saturation |
o the zone of soil
moisture |
o the water table |
o the capillary
fringe |
o the unsaturated
zone |
Part D
During a summer with
little rainfall, your house on a hill slope experiences an interval during
which your well runs dry. You have to borrow water from your neighbour who
lives down slope from you. Why does your neighbour have water when you don’t?
As the water table
drops due to the lack of precipitation, it goes below the base of your well. |
o Your neighbour is
drawing the water away from your well. |
o The zone of
saturation has risen at your neighbour’s house. |
o As the water table
goes below your well, it is going up at your neighbour’s. |
o The zone of soil
moisture has risen at your neighbour’s house. |
Question Attachments
0 attachments —