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A great view showing the basalt base underlying Smith Rock State Parka and the browns and reds of the top layer of rocks that were formed from welded tuff and rhyolite rocks. The welded tuff was formed from ash that was melted together as it fell onto the

aaw.jpg The striations in the rocks suggest the land was tilted in some past geologic time.ThumbnailsMore rock spires at Smith Rock State Park provide for great scenery as you hike through the park.The striations in the rocks suggest the land was tilted in some past geologic time.ThumbnailsMore rock spires at Smith Rock State Park provide for great scenery as you hike through the park.The striations in the rocks suggest the land was tilted in some past geologic time.ThumbnailsMore rock spires at Smith Rock State Park provide for great scenery as you hike through the park.The striations in the rocks suggest the land was tilted in some past geologic time.ThumbnailsMore rock spires at Smith Rock State Park provide for great scenery as you hike through the park.The striations in the rocks suggest the land was tilted in some past geologic time.ThumbnailsMore rock spires at Smith Rock State Park provide for great scenery as you hike through the park.The striations in the rocks suggest the land was tilted in some past geologic time.ThumbnailsMore rock spires at Smith Rock State Park provide for great scenery as you hike through the park.The striations in the rocks suggest the land was tilted in some past geologic time.ThumbnailsMore rock spires at Smith Rock State Park provide for great scenery as you hike through the park.

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Author
Steve Jones
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