Gneiss with Joint Control of Stream Rock Deposit
Large scale gneiss-like banding can be seen in the parallel ridges and valleys oriented photographically vertical in thumbnail 1. Cross banding joints are responsible for the angular stream habit (meanders) shown in thumbnail 2.
-
Base
photo in low resolution with LINKED locations of high resolution
3D images (10s of kb)
-
Base
photo in medium resolution to allow exploration of gray tone detail
(100s of kb)
-
Three dimensional anaglyph photo at 1200 dpi ( MBs JPEG file that will
expand to 10s of MB)
-
Three dimensional illustration of the deposit
-
Photo of typical cross section
-
Example of typical quantitative characterization data
Home