Wikiplacemarks.com  
 



Find us on Google+

Purgatory Chasm outcrop

View on map:41.486812°N 71.268011°W

Comments

The Purgatory Conglomerate is of lower Paleozoic and consists of quartzite.  The deformation is due to pressure solution of these aluvial fan deposits.    

References

Average user rating: Not rated

Click on a star to rate
 
您有一個表格您想把它變成應用程序嗎？
請與我們分享您的意見。