Chapter 2: Problem 9
Dust collecting on furniture is an everyday example of a sedimentary process. Provide another example of a sedimentary process that might be observed in or around where you live.
Short Answer
Expert verified
Sediment accumulating at the base of a drainpipe is an example of a local sedimentary process.
Step by step solution
01
Understanding Sedimentary Processes
A sedimentary process involves the accumulation and compaction of particulate matter, typically originating from weathering and erosion of rocks. These processes can occur naturally in environments like rivers, lakes, and oceans where sediments are deposited over time.
02
Identifying Local Sedimentary Processes
To find another example of a sedimentary process in your area, consider places where water or wind can transport and deposit materials. This might include riverbanks, beaches, or even urban environments where particles settle in corners and crevices.
03
Selecting a Specific Example
In a common urban or suburban setting, one example could be the formation of sediment at the base of a drainpipe. Rainwater can carry soil and debris from various surfaces to a specific low point, where the materials settle and accumulate over time.
04
Describing the Process
The rainwater flows across surfaces like roofs, collecting particulates and organic matter. This mix is transported via gutters and downspouts and ultimately accumulates at the bottom of the drainpipe, forming a small sediment deposit.
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Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Sediment Deposition
Sediment deposition is the process where materials, referred to as sediments, settle out of air or water flow to accumulate in a particular area. This process is crucial in forming features such as deltas, sand dunes, and oceanic floors. Sediments can include tiny particles like silt, sand, and clay, all the way up to larger debris such as gravel and boulders.
Deposition occurs when the carrying agent, like water or wind, loses energy and can no longer support the weight of sediments. As the speed of water or air decreases, the heaviest particles settle first, followed by progressively lighter materials.
Deposition occurs when the carrying agent, like water or wind, loses energy and can no longer support the weight of sediments. As the speed of water or air decreases, the heaviest particles settle first, followed by progressively lighter materials.
- In rivers, slowing the flow leads to sediment buildup, creating riverbanks.
- On beaches, tides distribute sand and organic debris along the shore.
Weathering and Erosion
Weathering and erosion are pivotal processes that break down rocks and transport sediments, respectively. Weathering is the breakdown of rocks and minerals into smaller particles through physical, chemical, or biological means.
- Physical weathering occurs through temperature changes, freeze-thaw cycles, or mechanical forces like wind and water.
- Chemical weathering involves reactions like oxidation or acid rain altering the mineralogical composition of rocks.
- Biological weathering happens when plants or animals contribute to rock disintegration.
Urban Sediment Accumulation
Urban sediment accumulation is the gathering of particles in city environments as a result of various activities and natural processes. Unlike natural settings, urban areas have increased impervious surfaces like roads and buildings, which can affect how sediments are distributed and deposited.
As rainwater washes over roofs, streets, and other surfaces, it collects particles and debris from various sources. These materials can include:
As rainwater washes over roofs, streets, and other surfaces, it collects particles and debris from various sources. These materials can include:
- Dust and dirt from construction sites and roadways.
- Organic matter such as leaves and small plants.
- Pollutants from vehicles and industrial activities.