The Earliest Geological Map of California
This is an important early geological map of California, prepared to accompany reports regarding the Transcontinental Railroad. The map is color-coded according to geological features, with a key provided in the lower left. The geology is shown west of the Great Western Divide, extending as far north as Grass Valley, and down to the Gulf of California. The detail on this subject is simple when compared to modern geologic maps, but surprising for the time and for the most part correct. This is truly a marvelous map of California.
The geology of the area is broken down into nine strata. The geology can be seen to range from the "granitic and metamorphic" rocks of the Sierra Nevada, which give the range its famous grey color, to the alluvium and other quaternary sediments found in the San Joaquin Valley. Basaltic flows are recognized near the westernmost part of the Sierra Nevada, just north of Fresno, and near Punta de Los Reyes. Perhaps most interestingly, from a geological standpoint, are the "serpentine traps" noted in such locations as San Francisco and Mt. Diablo. For the most part, these are degraded ophiolites, meaning that these were parts of the seafloor, originally erupted 10,000 ft. below the surface of the ocean, which have been thrust onto land during the formation of California. They were originally composed of basalt and peridotite (this latter is basalt that has crystallized at depth), but the thrusting process introduced to water, which broke down the crystal structures of the minerals and converted the rock into serpentinite. This is a major source of natural asbestos.
Most of the geological groupings have interesting have additional notes, for example alluding to the basaltic deposits of the Cascades or drift of the Great Basin. It is impossible to understate the importance of geology in California's history, which early explorers would have recognized. This influences everything from mining in eastern California, to landslides in San Francisco, to agriculture in the central valley, and to the location of mountain passes through the Sierra Nevada.
Regarding non-geological detail, the surveying on the map was at the forefront of its field, though the map lacks some major details. Tahoe is but a tiny lake named Bonpland, dwarfed by Mono Lake and other lakes in the region. The rivers of Southern California are well-demarcated, and several westward routes are marked heading to San Diego and Los Angeles over Warner and Cajon passes. The Coast ranges are still little mapped, with no peaks appearing. Oakland was incorporated between surveying and publication of the map, making it one of the earliest state-wide maps to show the city. Another area of interest is the mining towns to be found on the western foothills of the Sierra Nevada.
The California Department of Conservation cites this as the "first geologic map that specifically and exclusively pertained to California." Earlier maps had focused on tiny parts of the state, for example, Edward Belcher's well-executed map of San Francisco published in 1839. Earlier geologic maps of the United States had touched on California, but this was extremely limited. For example, Hildburghausen in 1853 simply colors the central valley yellow, marks it as a gold region, and eschews any other detail. The second map of the state following Blake's would not appear until 1867, and several other independently published maps would continue until the first California geologic survey map of 1891.
This map was published alongside several other attempts by the U.P.R.R. focusing on specific parts of the state, and so far we have been able to locate detailed mapping of San Francisco and of the Coast Ranges from Los Angeles northwards.
The Pacific Railroad Surveys
This work was produced by William Phipps Blake, a "Yankee Gentleman and Pioneer Geologist of the Far West" (Dill) during the Pacific Railroad Surveys of 1853. These were a series of five surveys that took place along several routes during the years 1853 to 1855 and were conducted in order to gather valuable information regarding possible routes of a transcontinental railroad. Four surveys followed east-west routes, comprised of a Northern Pacific, Central Pacific, and two Southern Pacific surveys. The fifth survey followed a north-south route instead, going from San Diego to Seattle. This is the survey that Blake was attached to and was led by Lt. Robert S. Williamson. This map was likely included in the 1857 publication by Theodore Judah which collated the information collected from the five surveys.
Blake, a Yale graduate and relative of Eli Whitney, was attached to the Williamson survey. He was a proficient mineralogist whose first job was to collect minerals for the New York City world fair prototype. He left this role less than a year after his graduation to join the 1853 Pacific Railroad Survey at the age of 26. At first, he was assigned to a party which surveyed half a dozen unsuitable passes throughout the Sierras, and he was sent on an unhopeful quest to survey a legendary pass in southern California. Blake would cement his importance in the survey when he discovered the excellent San Gorgonio Pass, which had, as of then, not appeared on any maps. After this thrilling discovery, Blake would explore the rest of the Colorado Desert before being sent northwards to explore the Coast Ranges. Blake would return to the East but soon realize that he was happier in California, where he would decamp and spend most of his life exploring, usually in a steep professional rivalry with his longtime colleague Josiah Whitney.
William Phipps Blake: Yankee Gentleman and Pioneer Geologist of the Far West. David B. Dill (1991)
The twelve-volume work Reports of Explorations and Surveys to Ascertain the Most Practicable and Economical Route for a Railroad from the Mississippi River to the Pacific Ocean, commonly known as the U.S. Pacific Railroad Surveys, stands as one of the most comprehensive and ambitious survey projects of 19th-century America. Conducted between 1853 and 1855, the surveys were commissioned by the U.S. War Department to explore and document potential routes for a transcontinental railroad. The project was of immense logistical scale and engaged some of the foremost scientists, engineers, and cartographers of the period. Their work provided a meticulously detailed examination of the topography, geology, natural resources, and native populations of the vast western territories, producing a landmark study that shaped the expansion of American infrastructure and industry.
The U.S. Pacific Railroad Surveys encompassed five major exploratory routes across the western United States, each corresponding to different potential paths for the transcontinental railroad. These included surveys through the northern territories from the Great Lakes to Puget Sound, central and southern routes traversing the Rocky Mountains and Sierra Nevada, and a route running along the 32nd parallel near the Mexican border. The selection of these corridors was strategic, aimed at finding the most feasible passages across the varied landscapes while balancing the interests of northern, southern, and western states and territories. The territories explored ranged from the Great Plains, stretching through rugged mountain passes, to the arid deserts of the Southwest and the coastal lowlands along the Pacific, all meticulously recorded in reports, sketches, and maps.
The northernmost route, surveyed by Governor Isaac I. Stevens of Washington Territory, investigated a path from St. Paul, Minnesota, across the northern plains, through the Rocky Mountains at Marias Pass, and to Puget Sound. Stevens’ survey is especially notable for its contributions from naturalists like George Suckley and John G. Cooper, who meticulously cataloged the flora and fauna encountered. Additionally, Stevens was a proponent of indigenous cooperation, advocating negotiations with Native American tribes to establish safe passage along the proposed route.
In the central region, John W. Gunnison led an expedition through the 38th parallel, traveling from St. Louis across Kansas and Colorado, into the rugged terrain of Utah, and finally into the Sierra Nevada. Tragically, Gunnison was killed during a skirmish with local Native Americans, and the survey was completed by Lieutenant Edward Griffin Beckwith. Gunnison and Beckwith’s reports are particularly valuable for their surveys of the Wasatch Range and for the inclusion of detailed maps that influenced later routes through the Great Basin and Salt Lake Valley.
Further south, the survey of the 35th parallel was led by Lieutenant Amiel Weeks Whipple, who documented the region extending from the Arkansas River through New Mexico and Arizona to the Pacific Ocean. Whipple’s route traversed desert regions and rugged landscapes, including the Colorado River basin. Whipple's survey also notably included artists like Heinrich Balduin Möllhausen, whose depictions of the landscapes and indigenous communities provided visual insights that were critical for Eastern audiences.
The southernmost route, following the 32nd parallel along what would become the Southern Pacific Railway corridor, was led by John Pope and pursued a path from the Red River to the Rio Grande and through Arizona and Southern California. This survey was strongly supported by Southern legislators, as it followed a path that could support a southern transcontinental link and presented fewer winter weather challenges compared to the northern routes. The reports from this route highlighted the unique topography of the Sonoran Desert and the California coastal plains.
In addition to the geographic explorations, the project saw significant contributions from leading cartographers and naturalists who produced groundbreaking work in mapmaking and scientific documentation. The primary cartographer was Lieutenant Gouverneur K. Warren, who oversaw the integration of the collected data into comprehensive maps. Warren's meticulous maps synthesized data from all five routes, resulting in the production of some of the most accurate and detailed maps of the American West at the time. His work was instrumental in consolidating information on the vast, uncharted territories, transforming raw survey data into accessible and invaluable resources for future expeditions and developments.
Several artists, including Möllhausen and F.W. Egloffstein, a German-born topographer, provided a visual dimension to the Pacific Railroad Surveys. Egloffstein’s contribution was pioneering; he used photolithography to create shaded relief maps, an innovation that added depth and realism to the depictions of the western terrain. His maps, particularly of the Great Basin, are considered some of the earliest examples of printed relief maps, giving readers in the East a tangible sense of the rugged landscapes and the formidable task of constructing a railroad through such regions.
The Pacific Railroad Surveys ultimately represented a collaborative effort that blended military precision, scientific rigor, and artistic skill to document the vast American landscape. While the route eventually chosen for the transcontinental railroad would follow a central corridor through Wyoming, the surveys influenced the development of future transportation corridors and provided foundational knowledge about the American West.