QUESTION IMAGE
Question
7c review questions
- what process affects all rocks after they have formed? what kind of earth materials does this process create?
- how are sediments moved about?
- assume that sediments collect on the deep ocean floor at a rate of 3 cm per 1000 years. how old might the ocean floor be if sediments are 90 cm thick? is this a reasonable answer?
- describe and compare mesas and buttes.
- how are monadnocks different from most other erosional mountains?
- what kind of depositional mountains or hills is formed by wind?
- what is glacial till? give two ways that glaciers can move till.
- why are volcanoes considered depositional mountains?
- (true or false) some fossilized sand dunes seen in sandstone formations may have actually formed underwater.
For Question 3:
Step1: Identify the rate and total thickness
The rate of sediment collection is $3$ cm per $1000$ years, and the total thickness of sediments is $90$ cm.
Step2: Set up the proportion
Let $t$ be the time (in years). We can set up the proportion $\frac{3\ \text{cm}}{1000\ \text{years}}=\frac{90\ \text{cm}}{t}$.
Step3: Solve for $t$
Cross - multiply: $3t = 90\times1000$. Then $t=\frac{90\times1000}{3}= 30000$ years.
Step4: Evaluate reasonableness
The ocean floor is constantly being subducted in some areas (due to plate tectonics), so in areas where subduction is active, the ocean floor is much younger. However, in areas with little subduction, this could be a reasonable estimate of the minimum age (since sedimentation is a continuous process but other factors like subduction can remove sediment).
The process that affects all rocks after they form is weathering (and erosion). Weathering breaks down rocks into smaller particles. The earth materials created are sediments (through physical and chemical weathering and subsequent erosion and transportation of the broken - down rock material).
Sediments are moved about by agents of erosion such as running water (rivers, streams), wind, glaciers, and gravity (mass wasting like landslides can move sediments). These agents transport the sediment from the site of weathering to other locations.
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The ocean floor might be $30000$ years old. Whether it is reasonable depends on the tectonic setting (e.g., in non - subducting areas it can be reasonable, in subducting areas it is not as the ocean floor would be recycled).