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Geology of the Shenandoah National Park Region - Csmres Jmu ...

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A.<br />

C.<br />

D.<br />

s<br />

lope p o<br />

r file<br />

B<br />

B<br />

scale<br />

E<br />

R I DG OW<br />

F U<br />

R<br />

R<br />

B<br />

A<br />

A<br />

A<br />

E.<br />

UNDISTURBED<br />

BLOCK FIELD<br />

SURFACE<br />

27<br />

1<br />

B.<br />

2<br />

25<br />

Figure 17 A. Shattered tor (height ~10 m)<br />

Quartzite blocks break along A) bedding planes<br />

and B) joint planes. B. Quartzite columns<br />

displaced by cambering and toppling. The tilt <strong>of</strong><br />

<strong>the</strong> lines demonstrates <strong>the</strong> toppling <strong>of</strong> <strong>the</strong> nearly<br />

horizontal beds after cambering has opened<br />

and separated <strong>the</strong> blocks along joint planes. C.<br />

Prominent block slopes west <strong>of</strong> Blackrock<br />

summit. D. "Curious" ridge and furrow feature at<br />

<strong>the</strong> toe <strong>of</strong> <strong>the</strong> block slope shown in C. Note <strong>the</strong><br />

geologists for scale. Landform may be a<br />

protalus rampart. E. Excavation pit <strong>of</strong> boulder<br />

front individual numbered boulders are identified<br />

in Figure 18. The line marks <strong>the</strong> upper<br />

boundary <strong>of</strong> <strong>the</strong> excavation.<br />

3<br />

7<br />

4<br />

5<br />

PIT<br />

FACE<br />

6<br />

BASE<br />

OF<br />

PIT

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