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Table 1. Landscape Features and Geologic Setting Observations: Read the descriptions in your textbook (Chapter 15 Investigati
Chapter 15 Investigation Workshoot; page 2 Table 2. Potential for Slope Failure at Specific Sites For the sites listed below,


< ch15_slopes_work... Q Q Û To complete this worksheet, see the instructions in the textbook (Chapter 15 Investigation) Table
Chapter 15 Investigation Worksheet: page 2 Table 2. Potential for Slope Failure at Specific Sites For the sites listed below,
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1- It contain trees that are tipped over at odd angles. This feature is called creep. Its not the area for habitation. Debris flow can occur here.

2- Formed by resistant rocks of basalt. The jointed rocks are known as columnar joints. These are high angle rock bodies and rock fall can happen.

3- It is snow capped steep mountain with no such evidence of recent volcanism but fumes occasionally rises from the central crater. Rock, debris or snow avalanche can happen here. Debris avalanche because the mountain has got association with mud in its right flank.

4- These are large mass of rocks and other debris with hummocky topography. This debris cut across paths of streams originating from adjacent hills. Since this area is devoid of trees and soil only rock slide is dominant not debris flow or debris slide.

5- Gray mountains have wide spaced fractured planes of granite. They dip opposite the mountain and is prone to rock slide landslide, due to the fracture planes present.

6- It is an area of volcanic ash that has weathered to form clay, thats why its topography is undulating due to swelling and compacting of soil. The soil absorb water and evaporate them which makes the topography bumpy and fractures can be seen here.

7- It is a tilted limestone hill, terraces can be seen so this area is prone to debris slide, slump, and rock slide during rainy season as water percolates the soil and dissolves the calcium carbonate - present and weaken the rock layers.

8- The cliff at base is steep enough for rock fall. At the base of the tilted limestone hill chaotically scattered blocks of rocks can be seen which is not part of the underlying topography. Clearly it has dropped from the hill which makes it certain that rock fall has happened.

9- It is relatively safe zone for habitation, as the topography is smooth and the river is flowing below the topography, the river don't seem to carry enough water because if had carried this area would have been prone to seasonal flood.

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