January 28, 2010 8:49 am
Heavy rain washed away the snow, exposing some interesting features of the rock surface of area mountains. This morning’s snow is laying down a fresh palette for wildlife tracks.
As for the rocks, when I saw this, I wondered if it had been split by temperature extremes:
But what really happened is that the tooth-like calcium deposit was not solid like this rock:
Moisture filled in between the gaps of the calicium “teeth” of the first rock.
I’ve spent a great deal of time hiking two mountains located less than 10 miles from each other which are composed of different geological materials. One is conglomerate rock with distinct vegetation and evidence of glacial movement.
The bedrock on the other mountain is precambrian gneiss outcroppings with mica and feldspar inclusions along with embedded microcrystalline quartz.