By Kevin Hinchman

There is something quietly remarkable about the fact that the name Hinchman appears not only in the genealogical records of colonial America and the box scores of 1950s minor league baseball — but also in the bedrock geology of the Sierra Nevada mountains of California, in strata laid down roughly 150 million years ago during the Jurassic Period.
The Hinchman Formation is a formally recognized geologic formation in California, catalogued in the scientific literature and preserved in the Paleobiology Database. It sits within the Taylorsville region of northern California's Plumas County, in the eastern Sierra Nevada foothills, where a remarkable sequence of Jurassic-era rock layers tells the story of an ancient volcanic arc that once rose where the mountains now stand.
The United States Geological Survey's foundational bulletin on the Taylorsville region — one of the most detailed early surveys of California's complex geology — places the Hinchman Formation (designated symbol: Jh) as a key layer within the upper Jurassic sequence. The survey describes it as ranging from 500 to 2,300 feet thick, consisting of:
In the USGS stratigraphic column for Taylorsville, the Hinchman sandstone sits between the Foreman Formation above (up to 2,500 feet of gray shale) and the Blacknell sandstone below, as part of the broader Jurassic rock sequence that also includes the Mormon, Thompson, and Bicknell formations in the same region.
During the Jurassic Period — roughly 201 to 145 million years ago — what is now California bore no resemblance to the state we know today. The land that would become the Sierra Nevada was an active volcanic island arc, similar in character to the modern islands of Japan or the Philippines, sitting offshore of the North American continent. Volcanic eruptions were frequent. Shallow seas lapped at the edges of the arc. The supercontinent Pangaea had recently broken apart, and the Atlantic Ocean was just beginning to open.
The sediments that would eventually become the Hinchman Formation were deposited in this dynamic environment — tuffaceous (volcanic ash-rich) sands and conglomerates shed from erupting volcanoes, mixed with marine sediments, compressed over millions of years into the rock we find today. The fossils preserved in the broader Taylorsville sequence include marine invertebrates, trace fossils, and evidence of the ancient sea floor that once lay where the mountains now rise.
Geologic formations are typically named for a geographic feature nearby — a creek, a valley, a township — where the formation is best exposed or was first formally described. The Hinchman Formation almost certainly takes its name from a local geographic feature in the Taylorsville area that itself bore the Hinchman name, perhaps a ranch, a creek, or a landowner's property in Plumas County.
The Hinchman family had spread widely across the American West by the mid-19th century, following the routes of westward migration that took Quaker and Appalachian families from New Jersey and Kentucky into Ohio, Indiana, and eventually California. It is entirely plausible that a member of the Hinchman family settled in the Taylorsville region during the Gold Rush era (1848 onward) or in the decades that followed, leaving a name on the landscape that geologists later adopted when formally describing the rock sequence.
Whatever its specific origin, the result is the same: the Hinchman name is now permanently inscribed in the scientific literature of North American geology, attached to a formation that has survived earthquakes, erosion, and the relentless passage of deep time. The rock itself — tuffaceous sandstone laid down in a Jurassic sea — will outlast everything we know. And it carries our name.
Family members interested in exploring the connection further may find useful information in:
If any member of the Society has knowledge of Hinchman family settlers in Plumas County, California, or of the specific geographic feature that gave the formation its name, we would be very grateful to hear from you.
Mary Hinchman
May 30, 2026
Interesting. Learn something new every day.