Name:  _______________________________________________ Section:_______________________

part 1:  Cascade Range Volcanos

1.   Explain briefly how a caldera forms, and how a caldera is different from other types of volcanic craters.

Eruption empties the magma chamber beneath the mountain, which then collapses to leave a crater

2.   Use the topographic map in Figure 18.3 (Crater Lake) to determine the approximate diameter of Crater Lake, in miles.  Use the ratio scale to calculate the diameter.  Please show all your work.  (((5.25"(62500))/63360)=5.18 miles

 

 

3.   Determine the total depth of the crater in Figure 18.3 (i.e. the distance from the top of the rim to the bottom of the lake) by following the steps below.

a.   Approximately how deep is the water in Crater Lake, in feet?              ABOUT 2000'

highest elevation on crater rim (above sea level)

 

elevation of water surface (above sea level)

 
b.   Determine the local relief from the water level in Crater Lake to the top of the crater, in feet. 

depth

 

local relief

 
Examine the contour lines carefully to determine where the ridge defining the top of the crater is located.  Then look for the benchmark designating the highest point along the crater rim.

 

What is the highest elevation of crater rim?  8156' (HILLMAN PEAK)

What is the elevation of the water surface?  6176'

What is the local relief from the water level to the top of the crater?    1980'

c.   Using the answers to parts (a) and (b), what is the total depth of the crater, in feet? 3980'

4.   Use the topographic map of Mt. St. Helens (Figure 18.4) to measure:

a.   The diameter of the crater from rim to rim in an east-west direction, across the center of the lava dome, in miles.  1.25 miles

 

 

b.   The total depth of the crater from the highest point on the crater rim to the bottom of the crater, in feet.  ~2065’

 

 

5.   Use the topographic map of Capulin Mountain (Figure 18.5) to measure:

a.   The diameter of the crater from rim to rim in an east-west direction, in feet.

1350’

 

b.   The total depth of the crater from the highest point on the crater rim to the bottom of the crater, in feet.

~412’

 

6.   Crater Lake, formerly Mount Mazama, and Mt. St. Helens are both part of the Cascade Range, whereas Capulin Mountain, located in New Mexico, is not.  Compare the diameters and depths of the craters associated with these volcanoes.

                                         Crater Width                                  Crater Depth

Crater Lake                   5.18 mi                                          3980’

Mt. St. Helens              1.25 mi                                          2065’

Capulin Mountain        0.26 mi                                          412’

a.       Comparing the measurements of Crater Lake to Mt. St. Helens, is the crater at Mt. St. Helens most likely an example of a caldera or is it just a large crater?  Why?

It is a caldera, as the volume of ejecta was large and the central portion of the original mountain partially collapsed into the evacuated magma chamber

b.   What accounts for the large difference in size of the craters at Mt. St. Helens and Capulin Mountain? The partial emptying of the magma chamber at St Helens

7.   Determine the slope angle for Mt. St. Helens (Figure 18.4). 

a.   Select an index contour line that approximates the base of the mountain and determine its elevation.

                                                                  Approximate base elevation (feet)   4600’

b.   The highest elevation of the crater rim is 8365 feet and is marked with an “x”.  Use a ruler to draw a line from this point downhill to the southwest to the contour line you selected to approximate the base of the mountain.  Measure the length of this line in feet.

                                                                  Distance from rim to base (feet)     9082’

c.   Calculate the gradient in feet/foot.  .414556

 

 

d.   The inverse sine of this number will tell you the slope in degrees.

                                                                                          Slope in degrees     24.5º               

8.   Determine the slope angle for Capulin Mountain (Figure 18.5).  Follow the same procedure outlined in question 7, measuring from the highest point on the crater rim.

Highest elevation (ft) 8182’

Base elevation (ft)      7000’

Distance (ft)              3200’

Gradient (feet/foot)    .369375

Slope (degrees)          21.7º

9.   Compare your slope measurements (in degrees) for Mt. St. Helens and Capulin Mountain to those listed in Table 18.1.

a.   What type(s) of volcanoes have slopes similar to yours? Composite or cinder cone

b.   Based on all of the measurements taken so far, what type of volcanoes are these, shield volcanoes, composite volcanoes, or cinder cones?

      Crater Lake (Mount Mazama)   composite

      Mt. St. Helens                          composite

      Capulin Mountain                    cinder

10. a.   What type of landform is Red Cone (shown on the Crater Lake topographic map, Figure 18.3) according to the geologic map in Figure 18.6? PARASITIC CINDER CONE

 

b.   Where are two other examples of this type of landform on the topographic map (Figure 18.3? DESERT CONE, CRATER PEAK, WIZARD ISLAND

 

c.   What type of rocks are these cones composed of (Figure 18.6)? pumice, rhyolite

 

d.   Based on the geologic map in Figure 18.6, do you think these cones formed before or after the eruption that formed Crater Lake?  Why? Later; they are higher, and Wizard Island is within the lake

 

11. Examine the map of pumice deposits associated with Crater Lake (Figure 18.7).

a.   Based on the isolines showing the thickness of pumice fall, what was the prevailing wind direction at the time Mount Mazama erupted? southwesterly

 

b.   Examine the topography to the south and southeast of Crater Lake, and to the north and northeast of Crater Lake (Figure 18.3).  Which area is flatter, the area to the north and northeast, or the area to the south and southeast? North and northeast

 

c.   What might be the reason for this difference in topography?  Use Figures 18.6 (Geologic Map) and 18.7 (Pumice Map) to help answer this question, and think about what the topography to the north and to the south of Crater Lake might have been like prior to the eruption that created the lake. Burial by pumice ash

 

 

12. Figure 18.8 shows the ash fallout from the 1980 eruption of Mt. St. Helens.

a.   Based on the patterns shown on the map, what was the prevailing wind direction at the time of the eruption? Westerly in Washington, but northerly in the Rocky Mountains

 

b.   How does the thickness of ash fall from Mt. St. Helens compare to the thickness of pumice fall from Mount Mazama? Mazama was twice as thick

 

c.   Examine the stereo photos in Figure 18.9.  Describe the topography to the north of the blast zone (north of the light grey area). flatter

 

 

 

d.   What do you think this landscape to the north of Mt. St. Helens would look like had the ash fall from Mt. St. Helens been similar to that of Mount Mazama? Perhaps even more flat due to deeper burial

 

13. Figure 18.10 shows the tectonic setting of the Cascade Mountain Range.  What type of plate boundary is causing the volcanic activity in this region? Convergent (subduction zone upwarp)

 


 

Crater Lake, OR

 

Mt St. Helens, WA

 

Capulin, NM


figure 18.3 [Crater Lake topographic map]

 

FIGURE 18.3  USGS Topographic map

Crater Lake, Oregon

Original was1:62,500; this is a 3/4 reduction

contour interval = 50 feet
FIGURE 18.4 Mt. St. Helens topographic map

FIGURE 18.4  USGS Topographic map

Mt. St. Helens

Original was1:48,000; this is a 2/3 reduction

contour interval = 40 feet
FIGURE 18.5 Capulin Mountain topographic map

FIGURE 18.5  USGS Topographic map

Capulin Mountain, New Mexico

Original was 1:24,000; this is a 1/2 reduction

contour interval = 20 feet

Figure 18.6  Generalized Geologic Map of Crater Lake and Vicinity

Adobe Systems 

 



Figure 18.7  Map Showing Distribution Pumice Deposits from Mount Mazama

 

 




FIGURE 18.8  Mt. St. Helens 1980 Ash Fall Map

 

 

 

 

 

 


FIGURE 18.9  Stereopair of Mt. St. Helens

 

 

 

 

 


figure 18.10  Map showing the relationship of the major Cascade volcanoes to plate interaction offshore of western North America.  Numbers in parentheses are dates of the most recent large scale volcanic activity for each volcano.

 

 

 

 

 

 

 

 

 

 

 


Name:  _______________________________________________ Section:_______________________

part 2:  landscape alteration: Ship Rock, New Mexico

Use the topographic map of Ship Rock, NM (Figure 18.11) to answer the questions below.

1.   What type of volcanic landform is Ship Rock? VOLCANIC NECK

 

2.   a.   On the topographic map, find two long ridges, one extending to the south-southeast and one to the west of Ship Rock.  Highlight these two ridges on the topographic map.

b.   If you walked along the top of either of these ridges, would the top be smooth or irregular?  How did you figure this out? Irregular; the upper contours are not single enclosures

 

 

c.   What type of landform are these two ridges examples of? EXHUMED VOLCANIC DIKES (MORE RESISTANT THAN HOST ROCK)

 

3.   Examine the stereo-pair of Ship Rock.  On these photographs, north is to the left.  Rotate the topographic map (Figure 18.11) so that north is to the left.

a.   How many dikes can be seen radiating outwards from Ship Rock on the air photos? FIVE

 

b.   Examine the topographic map carefully and locate all the dikes which can be seen on the air photos.  Use the shape of the contour lines to help locate these dikes.  Highlight these remaining dikes on the topographic map.

4.   a.   On the air photos, just below and to the right (southwest) of Ship Rock, a cinder cone is evident.  Highlight this cinder cone on the topographic map.

b.   How do the contour lines show the cinder cone?  What shape do the contour lines have? CONCENTRIC CIRCLES

 

c.   There are three other distinct cinder cones in the photos.  Locate and highlight them on the topographic map.

 

5.   What is the approximate local relief of Ship Rock?

a.   Highest elevation                           7178'

b.   Lowest elevation (approximate):     5600'

c.   Local relief                                     1578'

6.   a.   What is the major process which has modified the landscape following the end of volcanic activity, producing the features evident today?

FLUVIAL EROSION

 

b.   Why has this process not erased all traces of the volcano that once existed here? SOLIDIFIED LAVA IS RESISTANT, AND FORMS A "CAP" PROTECTING THE UNDERLYING WEAKER SEDIMENTARY ROCK. SOME BURIED INTRUSIVE FEATURES ARE VERY DEEP, SO THAT EROSION OF THE SURROUNDING ROCK EXHUMES AND LEAVES THEM AS PROTRUDING LANDFORMS.

 

 


Insert Figure 18.11   [Ship Rock topographic map]


FIGURE 18.5  USGS Topographic map

Ship Rock, New Mexico

1:24,000

contour interval = 20 feet