Geology Reference
In-Depth Information
The study of granitic landforms and terrains well demonstrates the relationships between major
and minor forms. Thus, the origin and distribution of flared slopes are germane to the origin and
evolution of bornhardts. The analysis of granite forms involves the consideration of some of the
most dramatic and enduringly fascinating landscapes on Earth.
In this analysis, while personal views have not been suppressed, various, frequently opposed,
interpretations have been outlined. No theory can ever be regarded as established, if only because
the data on which it is based is incomplete or flawed. In our interpretations of various granite land-
forms we are enthusiastic and tenacious, but not dogmatic. While acknowledging the reality and
wry humour behind the comment, we could not go so far as Lichtenberg when he remarked: “
instead
of saying I have explained such and such a phenomenon, one might say, I have determined the causes
for it the absurdity of which cannot be conclusively proved
.”
Nevertheless, though the ideas presented appear soundly based in light of present data and con-
cepts, our greatest reward will be to stimulate others with different experiences and backgrounds
to formulate new explanations for the fascinating features found in granitic terrains. In this way,
new light will be shed not only on the features discussed in this topic, but on the evolution of
landscapes in general.
