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James Hall
-noted deformed Paleozoic strata in the Appalachians (10 times the thickness of undeformed Pal. strata in the Mississippi valley).
-Proposed Geosyncline Theory (until 1962)
Geosyncline Theory
Proposed by James Hall, pieces of underlying granite break off and promotes mountain building due to vertical sag and rise.
Antonio Snider-Pellegrin
First proposed that S. America and Africa were once connected.
J. D. Dana
-Proposed that continents floated in the mantle due to them being less dense, granitic material compared to more dense basaltic material.
-Proposed that Earth cooled form an initial molten mass.
-Enhanced Geosyncline Theory: realized sediments aren’t dense enough to compress crust.
-Accepted isostacy.
-Proposed use of kerosene for lighting city lamps instead of whale oil, indirectly “saving” blue whales.
Johann Steinman
Igneous Petrologist
-Discovered ocean crust: studied sequences of rock where ocean crust is thrusted onto continents (Ophiolite Sequence)
Andrija Mohorovic
-Discovered Mohorovich Discontinuity: used seismograms and found certain energy waves arrived sooner to recording tools than others and figured there is a boundary in different places.
**Average Thickness in NY: 30km
Alfred Wegener
Meteorlogist
Originally theorized the concept of continental drift, but idea was rejected and seen as propaganda since Germany was an aggressor in WWI
*No tools or mechanism to prove theory, denounce after WWI ended.
D. T. Griggs
-Proposed a slow-moving fluid stratum that pulls down crust to form trenches what we know as subduction.
H. H. Hess
-Published first paper for plate tectonics: “History of Ocean Basins (1962)”.
Hugo Benioff
-Set up tunnels in the bedrock of the San Andreas fault.
-Trailblazed the idea of subduction zones.