List of National Natural Landmarks in California
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From List of National Natural Landmarks, these are the National Natural Landmarks in California. There are 37 in total.[1]
More information Name, Image ...
Name | Image | Date | Location | County | Ownership | Description |
---|---|---|---|---|---|---|
Amboy Crater | May 1973 | 34°31′11.69″N 115°43′26.92″W | San Bernardino | Federal (Bureau of Land Management) | A 6,000-year-old volcanic cinder cone, made up of pahoehoe, just off historic U.S. Highway 66. | |
American River Bluffs and Phoenix Park Vernal Pools | 1976 | 38°39′10.33″N 121°12′59.95″W | Sacramento | Federal (United States Bureau of Reclamation), state (California State Parks), and municipal (Fair Oaks Recreation and Park District) | Contains vernal pools, and blue oak woodlands.[2] | |
Año Nuevo State Reserve | 1980 | 37°7′7.24″N 122°18′24.02″W | San Mateo | State (California Department of Parks and Recreation) | One of the largest mainland breeding grounds for the northern elephant seal.[3] | |
Anza-Borrego Desert | 1974 | 33°14′57.38″N 116°24′24.63″W | Imperial, Riverside, San Diego | State (California Department of Parks and Recreation) | The largest desert state park in the nation.[4] | |
Audubon Canyon | 1968 | 37°55′46.01″N 122°40′55.85″W | Marin | Private | The largest known nesting area for great blue herons and great and snowy egrets on the Pacific Coast.[5] | |
Black Chasm Cave | 1976 | 38°26′3.4″N 120°37′35.3″W | Amador | Private | A small three-level cave containing a variety of speleothems and some of the best helictite formations in the western U.S.[6] | |
Burney Falls | 1984 | 41°0′43.79″N 121°39′7″W | Shasta | State (California Department of Parks and Recreation) | Contains some of the best examples in the western United States of a river drainage regulated by stratigraphically controlled springs.[7] | |
Cinder Cone Natural Area | 1973 | 35°17′21.95″N 115°35′6.99″W | San Bernardino | Federal (Mojave National Preserve) | A complex of over 20 large cinder cones of recent origin with extensive and continuous lava flows.[8] | |
Cosumnes River Riparian Woodlands | 1976 | 38°15′56.57″N 121°26′21.22″W | Sacramento | Private, Federal, State, and County | A small remnant of a rapidly-disappearing riparian woodland community type that once formed a major part of the central valley.[9] | |
Deep Springs Marsh | 1975 | 37°20′00″N 118°01′03″W | Inyo | Private | An example of increasingly rare desert marsh.[10] | |
Dixon Vernal Pools | 1987 | 38°16′31.29″N 121°49′25.49″W | Solano | Private | The best example of valley needlegrass grassland in the central valley.[11] | |
Elder Creek | 1964 | 39°43′32.04″N 123°37′34.35″W | Mendocino | State (University of California Natural Reserve System) | A largely undisturbed watershed containing large old stands of Douglas fir, broadleaf evergreens, and deciduous trees.[12] | |
Emerald Bay | 1968 | 38°57′25.49″N 120°5′36.3″W | El Dorado | State (California Department of Parks and Recreation) | An outstanding example of glacial geology.[13] | |
Eureka Dunes | 1983 | 37°5′45.6″N 117°40′30″W | Inyo | Federal (Death Valley National Park) | The tallest dune complex in the Great Basin.[14] | |
Fish Slough Area of Critical Environmental Concern | 1975 | 37°28′8.69″N 118°24′3.1″W | Inyo, Mono | Mixed- federal (Bureau of Land Management), state, municipal | A large, essentially undisturbed, desert wetland that provides habitat for the alkali mariposa lily and the endangered Owens pupfish.[15] | |
Guadalupe-Nipomo Dunes | 1974 | 34°57′56.13″N 120°39′1.24″W | San Luis Obispo | Mixed- federal (Guadalupe-Nipomo Dunes National Wildlife Refuge), state, private | A coastal dune tract with off-road vehicle recreation, a national wildlife refuge, beaches, and nesting for the western snowy plover.[16] | |
Imperial Sand Hills | 1966 | 32°55′0″N 115°3′0″W | Imperial | Federal (Bureau of Land Management) | One of the largest dune patches in the United States.[17] | |
Irvine Ranch Natural Landmarks | 2006 | 33°43′53.4″N 117°41′34.8″W | Orange | Mixed- state, county, municipal | A remarkably complete stratigraphic succession ranging in age from late Cretaceous to the present.[18] | |
Lake Shasta Caverns | May 2012 | 40°48′16.2″N 122°18′15.98″W | Shasta | Private | A well-decorated Solutional cave that contains a diverse assemblage of calcite cave formations.[19] | |
Lanphere Dunes and Ma-le'l Dunes | 2021 | Humboldt | Federal (Bureau of Land Management, Humboldt Bay National Wildlife Refuge) | Considered to be the largest and best quality sand dune ecosystems representing coastal dunes in the area.[20] | ||
Miramar Mounds | 1972 | 32°50′43″N 117°8′19″W | San Diego | Federal (Marine Corps Air Station Miramar) | Contains unique soil features called mima mounds, which are found in only three or four locations in the country, and vernal pools.[21] | |
Mitchell Caverns and Winding Stair Cave | 1975 | 34°56′26.97″N 115°30′51.97″W | San Bernardino | State (California Department of Parks and Recreation) | Regarded as the most important solution caverns in the Mojave Desert.[22] | |
Mt. Diablo State Park | 1982 | 37°52′37.75″N 121°55′25.79″W | Contra Costa | State (California Department of Parks and Recreation) | One of the few areas in the region where geologic strata of Jurassic, Cretaceous, and Tertiary age can be seen in an aggregate thickness of 42,000 feet (13,000 m).[23] | |
Mount Shasta | 1976 | 41°24′35.6″N 122°11′41.52″W | Siskiyou | Federal (Shasta-Trinity National Forest) | One of the world's largest and most impressive stratovolcanoes, within the Shasta-Trinity National Forest.[24] | |
Pixley Vernal Pools | 1987 | 35°59′3.85″N 119°12′45.04″W | Tulare | Private | One of the few remaining natural vernal pools containing rare endemic crustacean species such as vernal pool fairy shrimp.[25] | |
Point Lobos | 1967 | 36°31′1.56″N 121°56′33.36″W | Monterey | State (California Department of Parks and Recreation) | An outstanding example of terrestrial and marine environments in close association, and the only known habitat of Monterey cypress and variegated brodiaea.[26] | |
Pygmy Forest at Jug Handle State Natural Reserve | 1969
1973 |
39°22′29.3″N 123°47′22.15″W | Mendocino | State (California Department of Parks and Recreation) | Includes a five step ecological staircase on which a unique forest of low, stunted trees and shrubs is located.[27] | |
Rainbow Basin | 1966 | 35°1′46″N 117°2′12″W | San Bernardino | Federal (Bureau of Land Management) | Deep erosion canyons with rugged rims with fossil evidence of insects and Miocene mammals.[28] | |
La Brea Tar Pits (Rancho La Brea) | 1964 | 34°3′46.62″N 118°21′21.49″W | Los Angeles | Municipal (City of Los Angeles) | Site of the world-famous natural asphalt tar pits.[29] | |
San Andreas Fault | 1965 | San Benito | Private | One of the best illustrations of earth displacement caused by small crustal movements.[30] | ||
San Felipe Creek Area | 1974 | 33°10′11″N 115°49′19″W | Imperial, San Diego | Federal (Bureau of Land Management), state (California Department of Fish and Wildlife) | A marsh containing probably the last remaining perennial natural desert stream in the Colorado Desert region.[31] | |
Sand Ridge Wildflower Preserve | 1984 | 35°18′31.26″N 118°47′24.29″W | Kern | Private | A remnant natural area displaying a great diversity of floral species including the Bakersfield cactus.[32] | |
Sharktooth Hill | 1976 | 35°26′30.57″N 118°56′26.18″W | Kern | Private | One of the most abundant, diverse and well- preserved fossil marine vertebrate sites in the world.[33] | |
Tijuana River Estuary | 1973 | 32°33′7.2″N 117°7′9.59″W | San Diego | Federal (Tijuana River National Estuarine Research Reserve), state, municipal | One of the finest remaining saltwater marshes on the California coastline.[34] | |
Torrey Pines State Reserve | 1977 | 32°54′59.58″N 117°14′58.7″W | San Diego | State (California Department of Parks and Recreation) | Contains a natural Torrey pine forest, high bluffs and sea cliffs, and endangered bird species.[35] | |
Trona Pinnacles | 1967 | 35°37′3.81″N 117°22′5.08″W | San Bernardino | Federal (Bureau of Land Management) | A relict landform from the Pleistocene containing unique formations of calcium carbonate.[36] | |
Turtle Mountain | 1973 | 34°19′5.53″N 114°51′7.28″W | San Bernardino | Federal (Bureau of Land Management), state | Contains two mountain sections of entirely different composition.[37] | |
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