Chapter 14: Problem 22
Notice that the Towaliga River Flows south, based on the position of the waterfalls, the rocks upstream are _________ to weathering while the rocks downstream are _________ to weathering . a. more resistant, less resistant b. less resistant, more resistant
Short Answer
Expert verified
Rocks upstream are more resistant to weathering, and rocks downstream are less resistant.
Step by step solution
01
Understanding Direction and Impact
First, understand the problem context. The Towaliga River flows south, which means the flow of water moves from north to south. Waterfalls often occur where the river encounters resistant rocks. This knowledge will help determine the relative resistance of rocks upstream versus downstream.
02
Analyzing Rock Resistance at the Waterfalls
The presence of waterfalls suggests that the rocks upstream (where the waterfalls are located) are resistant, as the river has not eroded them away. Waterfalls are typically formed where the river encounters hard, resistant rock that wears away slowly.
03
Assessing the Downstream Rock Condition
Downstream of the waterfalls, the rocks tend to be less resistant. This is why they're more easily eroded, allowing sediment to be carried downstream and leading to a smoother riverbed. The absence of waterfalls in this region supports the idea that these rocks offer less resistance than those upstream.
04
Conclusion from Analysis
Based on the analysis, rocks upstream (at the waterfalls) are more resistant to weathering, whereas rocks downstream are less resistant due to more erosion.
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Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Weathering
Weathering is the process that breaks down rocks into smaller pieces. It can happen in different ways, ranging from physical to chemical processes. Weathering makes the rock surface break apart and crumble over time.
There are two main types of weathering:
There are two main types of weathering:
- Mechanical Weathering: This involves the physical breakage of rocks without changing their chemical structure. An example would be freeze-thaw cycles, where water seeps into cracks, freezes, and expands, causing the rock to split.
- Chemical Weathering: This involves a chemical transformation of rocks. Acids and water reacting with minerals in the rocks lead to decomposition or alteration. An example is oxidation, where iron in the rock reacts with oxygen to form rust.
River Erosion
River erosion is a natural process that changes the landscape as rivers carve through rock and soil. As water flows, it erodes the material in its path. This process can reshape valleys and create new landforms over time.
River erosion happens in various ways:
River erosion happens in various ways:
- Hydraulic Action: The force of water alone can erode softer materials along the riverbank.
- Abrasion: Rocks and sediment within the water scratch and wear down the riverbed and banks.
- Attrition: Sediments crash into one another, becoming smaller and rounder over time.
- Solution: Water dissolves soluble minerals from the riverbed, deepening the channel.
Rock Resistance
Rock resistance refers to how well rocks withstand weathering and erosion. Different rock types have varying levels of resistance based on their mineral composition and structure.
Here are some factors influencing rock resistance:
Here are some factors influencing rock resistance:
- Composition: Harder minerals like quartz make rocks more resistant.
- Texture: Dense and fine-grained rocks resist erosion better than porous or coarse-grained ones.
- Weathering Patterns: Rocks with fewer cracks are more durable as cracks often serve as pathways for water and chemical agents.
Waterfalls
Waterfalls are stunning natural features that occur where rivers encounter areas of hard, resistant rock. The water cascades down the rock face, creating a dramatic drop.
Here's how waterfalls form:
Here's how waterfalls form:
- When a river flows over a layer of hard rock on top of softer ground, it begins to erode the softer material beneath, undercutting the harder rock.
- Over time, the support for the top layer crumbles, causing it to collapse into the plunge pool below, where the process begins again.
- This sequence creates the steep and often dramatic drop characteristic of waterfalls.