Acidic Erosion of Granite
This photo shows erosion
channels that developed in the rock underneath a
blanket of moss on Wheeler Mountain in northern
Vermont.
Wheeler Mountain and neighboring mountains in northern
Vermont are granite batholiths - solid granite that
forms dome-like mountains. Granite consists of quartz
(SiO2), feldspars (KAlSi3O8),
and mica. Mica with the feldspars is the
predominant mineral. This area of the mountain
had been covered with a thick layer of moss that had
"recently" disappeared - perhaps in the past half
century. Druing the many years that moss covered
the rock, the dead organic matter in the moss layer
tended to make the percolating rainwater slightly
acidic, thus dissolving some of the rock, namely the
feldspars, that are susceptible to acids.

The large mottled appearance of the rock surface is due
to the flacking of 2-3 cm diameter chips of the granite
due to rain, and repeated freezing and thawing during the
long, severe winters. The actual individual
crystallites of the feldspars are actually much smaller -
1-2 mm diameter as revealed by the texture in the erosion
channel.
The photo at right shows a larger field of view of the
area. The edge of existing moss can be seen in the
top of the photo.
My thanks to WWC geologist Robert Hastings for information
on the properties and composition of feldspars.
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