Final Group Activity
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| Figure 1.0— Full Image of Peyto Lake |
When I first examined Figure 1, I realized there were a lot more geological features than i first realized.
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| Figure 2,0 – Unique Turquoise lake of Peyto Lake |
The first thing I noticed in Figure 2.0 was how there was a unique color to Peyto Lake. I’m not exactly sure what may cause this turquoise color, but I believe it may have something to do with the glacier next to it. I would like to say that the glacier is what is giving the lake its color because it’s the source of the water.
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| Figure 2.1— Glacier of Peyto Lake |
This is another geological observation I noted. The glacier I observed of Peyto Lake; It fascinates me to observe how this glacier goes into the lake.
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| Figure 3.0—Sedimentary Rock |
I thought Figure 3.0 to be a sedimentary rock because the particles may have originated from the weathering of the other rocks in the area.
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| Figure 3.1—Weathering |
Figure 3.1 was geological observation of weathering. The mountain is currently covered in snow which could affect it.
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| Figure 4.0—Igneous Rock: Granite |
In all honesty, I was a bit hesitant observing Figure 4.0 to be granite. But I believe it to granite because the rocks look coarsely grained.
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| Figure 5.0- Metaphoric rock |
Figure 5.0 looks like metaphoric rock because of the way the pressure, perhaps air pressure
(?) may have morphed the rock.
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| Figure 6.0 left side of picture |
Figure 6.0 display cliffs because of the contour lines between both elevation of the mountains
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Figure 7.0 on the glacier, towards the water
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Figure 7.0: This is a glacier till because the glacier ice melts and drops its load of rock fragments
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