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The Earliest Printed Map of the Salton Sea
Extensively Annotated by George Ruhlen
Fine early map of the Salton Sea area, published shortly after flooding from the Colorado River and poorly designed irrigation canals caused the flooding of what had previously been the town of Salton and vicinity, creating one of the largest inland lakes west of the Mississippi River over the course of several years in the first decade of the 20th Century.
The map was first issued in 1906, shortly after the Salton Sea was created, and updated in 1907 and 1908, by which time the Salton Sea had further grown and changed shape. The present example one of the early updated versions, styled "reprinted, April 1908."
History of the Salton Sea
The area was once part of a vast inland sea that covered a large area of Southern California. Geologists estimate that for three million years, at least through all the years of the Pleistocene glacial age, a large delta was deposited by the Colorado River in the southern region of the Imperial Valley. Eventually, the delta reached the western shore of the Gulf of California, creating a barrier that separated the area of the Salton Sea from the northern reaches of the Gulf. Were it not for this barrier, the entire Salton Sink along with the Imperial Valley would be submerged as the Gulf would extend as far north as Indio.
Evidence that the basin was occupied periodically by multiple lakes includes wave-cut shorelines at various elevations preserved on the hillsides of the east and west margins of the present lake, the Salton Sea.
Throughout the Spanish period of California's history, the area was referred to as the "Colorado Desert" after the Colorado River. In a railroad survey completed in 1855, it was called "the Valley of the Ancient Lake". On several old maps from the Library of Congress, it has been found labeled "Cahuilla Valley" (after the local Native American tribe) and "Cabazon Valley" (after a local Native American chief – Chief Cabazon). "Salt Creek" first appeared on a map in 1867 and "Salton Station" is on a railroad map from 1900, although this place had been there as a rail stop since the late 1870s. Until the advent of the modern sea, the Salton Sink was the site of a major salt-mining operation.
In 1900, the California Development Company began construction of irrigation canals to divert water from the Colorado River into the Salton Sink, a dry lakebed. After construction of these irrigation canals, the Salton Sink became fertile for a time, allowing farmers to plant crops.
Within two years, the Imperial Canal became filled with silt from the Colorado River. Engineers tried to alleviate the blockages to no avail. In 1905, heavy rainfall and snowmelt caused the Colorado River to swell, overrunning a set of headgates for the Alamo Canal. The resulting flood poured down the canal, breached an Imperial Valley dike, and ran down two former dry arroyos: the New River in the west, and the Alamo River in the east. Over about two years, these two newly created rivers sporadically carried the entire volume of the Colorado River into the Salton Sink.
The Southern Pacific Railroad tried to stop the flooding by dumping earth into the canal's headgates area, but the effort was not fast enough, and the river eroded deeper and deeper into the dry desert sand of the Imperial Valley. A large waterfall formed as a result and began cutting rapidly upstream along the path of the Alamo Canal that now was occupied by the Colorado. This waterfall was initially 15 feet high but grew to 80 feet high before the flow through the breach was stopped. Originally, it was feared that the waterfall would recede upstream to the true main path of the Colorado, becoming up to 100 to 300 high, at which point it would be practically impossible to fix the problem.
As the basin filled, the town of Salton, a Southern Pacific Railroad siding, and Torres-Martinez Native American land were submerged. The sudden influx of water and the lack of any drainage from the basin resulted in the formation of the Salton Sea.
Provenance
Colonel George Ruhlen (1884-1971), noted Southern California historical geographer.
Manuscript Annotations
Ruhlen has marked out (with pencil dotted lines and red pencil) several historical routes through the region, including toponyms on both sides of the U.S.-Mexico boundary: Kearny, Emory, Butterfield Mail Route, Railroad Survey, New River, Gardner's Well Station, Ft. Yuma, Norton's Well, Indian Wells, Cooke's Well, Hall's Well.
Rarity
This map is scarce in the market.
Colonel George Ruhlen (1884–1971) was a distinguished military officer and historical geographer whose career spanned significant developments in U.S. military history, particularly during the early and mid-20th century. Best known for organizing the coastal defenses of San Diego after Pearl Harbor, his leadership, particularly during World War II, and his contributions to historical scholarship made him a respected figure in both military and academic circles.
Born at Fort Totten, near Devil's Lake, North Dakota, in 1884, Ruhlen came from a family with a deep military tradition. His father, Major General George Ruhlen, was a U.S. Army quartermaster. Ruhlen graduated from the United States Military Academy at West Point and was commissioned as an officer in the U.S. Army. His early postings were within the Quartermaster Corps, but over time, he transitioned to roles of increasing responsibility within the field artillery, where he demonstrated keen leadership skills. His career saw him stationed at various posts, with a notable assignment in 1938 as the commanding officer of Corregidor, a fortress island in the Philippines critical to the defense of Manila Bay.
Colonel Ruhlen is perhaps best remembered for his role as the commander of Fort Rosecrans, a key military installation in San Diego, California. After the attack on Pearl Harbor on December 7, 1941, Ruhlen was tasked with organizing the coastal defenses of San Diego, a city that was seen as vulnerable to Japanese attack in the early days of the Pacific War. Fort Rosecrans, located on the Point Loma peninsula, became the centerpiece of Ruhlen’s efforts to fortify the region.
In his capacity as commander, Ruhlen oversaw the deployment of coastal artillery and anti-aircraft defenses, ensuring that San Diego, a vital Pacific Fleet base and a hub for wartime logistics, was well-protected. His leadership during this period was crucial in maintaining the security of one of the most strategically important cities on the U.S. West Coast.
Ruhlen retired from the U.S. Army in 1944, but his contributions to the San Diego community did not end there. He became heavily involved in historical research and preservation, notably serving as the president of the San Diego Historical Society during the late 1940s and early 1950s. In this role, Ruhlen was instrumental in promoting the study of Southern California's military history, especially the role that Fort Rosecrans and other installations played in the defense of the region during World War II.
Ruhlen’s work as a historical geographer extended beyond military history. He was particularly interested in the history of the American West and the strategic role of military forts in the development of the region. His research and writings contributed to a greater understanding of the military’s influence on the growth of Southern California, helping to preserve the legacy of the region's military past.
Colonel George Ruhlen was part of a family with a remarkable military lineage. His father, George Ruhlen Sr., served as an Army inspector general and was a significant figure in the U.S. Army during the early 20th century. Ruhlen's son, also named George Ruhlen, followed in his father’s and grandfather’s footsteps, serving with distinction in the U.S. Army during World War II. As a Lieutenant Colonel, George Ruhlen III commanded the 3rd Armored Field Artillery Battalion, a unit of the 9th Armored Division that played a key role in halting German advances during the Battle of the Bulge, particularly in the defense of Medernach.
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