The Kreyenhagen Hills are a range of
foothills
Foothills or piedmont are geographically defined as gradual increases in elevation at the base of a mountain range, higher hill range or an upland area. They are a transition zone between plains and low relief hills and the adjacent topograp ...
of the
Diablo Range
The Diablo Range is a mountain range in the California Coast Ranges subdivision of the Pacific Coast Ranges in northern California, United States. It stretches from the eastern San Francisco Bay area at its northern end to the Salinas Valley are ...
in western
Fresno County and
Kings County Kings County or King's County may refer to:
Places Canada
*Kings County, New Brunswick
*Kings County, Nova Scotia
*Kings County, Prince Edward Island
** King's County (electoral district), abolished in 1892
Ireland
* County Offaly, formerly call ...
,
California
California is a U.S. state, state in the Western United States, located along the West Coast of the United States, Pacific Coast. With nearly 39.2million residents across a total area of approximately , it is the List of states and territori ...
.
The Kreyenhagen Hills form a long foothill belt in the soft formations between
Reef Ridge
A reef is a ridge or shoal of rock, coral or similar relatively stable material, lying beneath the surface of a natural body of water. Many reefs result from natural, abiotic processes— deposition of sand, wave erosion planing down rock ou ...
and
Kettleman Plain. They are divided into several groups, each a few miles wide, by streams crossing them at right angles. They meet with the steep face of Reef Ridge, and are distinct from the mountains which begin there. To the northeast the strata form ridge after ridge, parallel to each other, and extend the length of the separate divisions between the main stream valleys. These ridges, appear like a series of waves advancing, toward Reef Ridge, and elsewhere to broken waves, as in a choppy sea. The ridges are slightly asymmetric, the northeast flank being a dip slope and fairly smooth, while the southwest flank is a steeper, strike face that is in many places eroded so as to leave sharp gullies and conical intermediate ridges extending outward. The groups of hillocks so produced bear some resemblance to an encampment of tents or huts, and the name ''Jacalitos'', (meaning the little huts), may have been applied to
Jacalitos Creek owing to this feature of the hills through which it flows. The greatest symmetry of the parallel ridges appear's in the portion of the Kreyenhagen Hills between Jacalitos Creek and
Big Tar Canyon, and there the long, straight, smooth troughs between the ridges doubtless gave rise to the name ''Canoas'', meaning trough, applied to
Canoas Creek which passes across the central portion of the hills.
[Ralph Arnold, Robert Anderson, DEPARTMENT OF THE INTERIOR, UNITED STATES GEOLOGICAL SURVEY, GEORGE OTIS SMITH, DIRECTOR, BULLETIN 398, GEOLOGY AND OIL RESOURCES OF THE COALINGA DISTRICT, CALIFORNIA, WITH A REPORT ON THE CHEMICAL AND PHYSICAL PROPERTIES OF THE OILS BY IRVING C. ALLEN, G.P.O., Washington, 1910, p.35-36] Kreyenhagen was the name of the family who originally owned the land in the area.
In the northern group of the Kreyenhagen Hills, the slope toward Jacalitos Creek on the northwest is steeper and shorter than that toward
Zapato Chino Creek on the southeast. The major part of the drainage flows in the latter direction. In the groups of hills between the other streams farther south such a feature is not so clearly to be made out, but it is true that the course taken by the drainage is predominantly toward the southeast. Toward the south the Kreyenhagen Hills become more worn, decline in elevation, and lose their relief. Prominent individual features are absent, and the foothill area is a rolling surface with low ridges and broad drainages sloping gradually toward and merging with the Kettleman Plain.
References
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Mountain ranges of Fresno County, California
Diablo Range
Geography of the San Joaquin Valley
Mountain ranges of Northern California