U.S.G.S. engineer Bailey Willis (†
February 19, 1949) was known for his unorthodox approach to geological
questions. Puzzled by the geological structures he discovered in
mountain ranges, long before computer-models were available, he
constructed a machine to simulate the mountain-forming process.
In a box with a moveable piston he
folded and crushed layers of beeswax and compared the structures with
the large tectonic folds and thrusts he had mapped in the Appalachian Mountains.
He realized that folds and nappes could form also by horizontal
movements and compressive forces – not, as still many geologists argued,
only by vertical movements.
Fig.1. Willis´”Compression Machine for Experiments” from “The Mechanics of Appalachian Structure” (1891).
Fig.2. Miniature
mountains made by the “compression machine” – the strata first form
regular folds, however as the shortening continues, shear zones develop
and single “tectonic nappes” start to pile up.
Fig.3. Folded
strata in the central Appalachian Mountains. In later years Willis
proposed a first version of plate tectonics to explain mountain
formation processes – the Atlantic Ocean was formed when a “bubble” of
magma pushed apart the American and European continents, along the borders the layers of rocks were compressed and folded up – the Appalachian Mountains formed. Unfortunately this mountain range is significantly older than the Atlantic…
Fig.4. Willis subdivided mountain ranges in a
central zone, characterized by folds, and an outer zone, characterized
by shear zones (geological map of Cleveland in Tennessee). Today we know
that the conformation can be much more complicated than that.
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