PACIFIC RAILROAD SURVEYS (1853–1854): GEOLOGIC INVESTIGATIONS OF WILLIAM PHIPPS BLAKE, THOMAS ANTISELL AND JULES MARCOU IN THE AMERICAN SOUTHWEST
Antisell attributed uplift of the Coast Ranges to two volcanic forces acting in opposition, directed northwards and southwards, that produced a rupture of the superficial strata, and a depression of the land below sea level, in the vicinity of San Francisco. Blake viewed the Rocky Mountains as previously deformed islands in Mesozoic seas and that the Triassic to Cretaceous deposits had been laid down around them, whereas Marcou interpreted the entire uplift simply as the result of a single orogeny, with multiple centers of upheaval and igneous intrusion. Their maps and geologic cross-sections were controlled with detailed topographic surveys addressing railroad grade. This poster provides the major geologic maps and profiles by Antisell, Blake and Marcou between the 34o and 36o N parallels, from the Mississippi River to Los Angeles and north to the Bay Area.