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The Massanutten Sandstone is a Silurian-aged quartz arenite that crops out in the center of the greater Shenandoah Valley. It is resistant to erosion, and holds up the ridges of the Massanutten mountain system. To explore the outcrop this was collected from, click here: gigapan.com/gigapans/113759 Image...
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- 111
- Explore Score
- 29
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Part of a series of GigaPans shot from this spot.
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- 325
- Explore Score
- 32
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The Massanutten sandstone is a Silurian-aged passive margin deposit that is correlative to the Tuscarora Formation of the western Valley & Ridge province. A bed is exposed here in a subvertical orientation along the Woodstock Tower Road, near its summit. Perspective is looking across strike to the west-northwest. Trace...
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- 317
- Explore Score
- 28
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The Massanutten sandstone is a Silurian-aged passive margin deposit that is correlative to the Tuscarora Formation of the western Valley & Ridge province. A bed is exposed here in a subvertical orientation along the Woodstock Tower Road, near its summit. Perspective is looking across strike to the west-northwest. Trace...
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- 0
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- Snapshots
- Total Views
- 312
- Explore Score
- 32
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The Massanutten sandstone is a Silurian-aged passive margin deposit that is correlative to the Tuscarora Formation of the western Valley & Ridge province. A bed is exposed here in a subvertical orientation along the Woodstock Tower Road, near its summit. Perspective is looking across strike to the west-northwest. Trace...
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- 1
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- Snapshots
- Total Views
- 401
- Explore Score
- 32
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The Massanutten sandstone is a Silurian-aged passive margin deposit that is correlative to the Tuscarora Formation of the western Valley & Ridge province. A bed is exposed here in a subvertical orientation along the Woodstock Tower Road, near its summit. Perspective is looking across strike to the west-northwest. Trace...
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- 0
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- Snapshots
- Total Views
- 328
- Explore Score
- 32
- Outcrop at the intersection of Fort Valley Road and Ramsey Road, Fort Valley, Virginia by Callan Bentley
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This area is mapped by Rader & Biggs (1976) as Mahantango Formation. Note pencil cleavage on breakdown slopes. Bedding is discernible in the most cleanly-exposed portion of the outcrop (center). Structural orientations (right-hand rule): Bedding: 205°, 25° Cleavage: 021°, 90° Image made as part of the Mid...
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- 0
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- Total Views
- 302
- Explore Score
- 31
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For comparison with another GigaPan from a few weeks ago: gigapan.com/gigapans/122528
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- 0
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- Total Views
- 277
- Explore Score
- 1
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For comparison with another GigaPan from a few weeks ago: gigapan.com/gigapans/122529
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Stats
- Favorites
- 0
- Comments
- Snapshots
- Total Views
- 378
- Explore Score
- 24
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For comparison with another GigaPan from a few weeks ago: gigapan.com/gigapans/122528
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Stats
- Favorites
- 0
- Comments
- Snapshots
- Total Views
- 280
- Explore Score
- 52

