The two perpendicular faces in the Tully Sandstone have resulted from erosion along the conjugate joint planes. This pattern of fractures is common in the Ithaca area.
|
|
The two perpendicular faces in the Tully Sandstone have resulted from erosion along the conjugate joint planes. This pattern of fractures is common in the Ithaca area. |
Send feedback with
questions or comments about this web site.
Copyright © 1998 - 2006, Ruth's Waterfalls of the Finger Lakes and Rochester,
NY, All rights reserved
Last modified: 28-Oct-2005