The Rice Fork
is a
[U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data]
The National Map
, accessed March 9, 2011 tributary of the
Eel River in
Lake County, California
Lake County is a county located in the north central portion of the U.S. state of California. As of the 2020 census, the population was 68,163. The county seat is Lakeport. The county takes its name from Clear Lake, the dominant geographic f ...
. The Rice Fork begins on the upper northwest side of Goat Mountain, on the
Colusa-Lake County line, at an elevation of over . It quickly descends the steep western slope of the mountain, then bends northward, and flows northwesterly down a narrow winding steep walled canyon for about , crossing two forest roads and adding many tributaries, ending its journey at the southern tip of
Lake Pillsbury
Lake Pillsbury is a lake in the Mendocino National Forest of Lake County, California, created from the Eel River and Hull Mountain watershed by Scott Dam. Elevation is with of shoreline and covering . Activities in the Lake Pillsbury Recreat ...
, at a varied elevation around , depending on the lake level. Before the construction of Scott Dam in the 1920s, which formed Lake Pillsbury, the Rice Fork ran directly into the Eel River. It is one of Lake County's longest streams.
The many tributaries to Rice Fork are Salt Creek, French Creek, Parramore Creek, Bevans Creek, Bear Creek, Packsaddle Creek, Willow Creek, Deer Creek, Rice Creek, and Soda Creek.
History
In the 1860s, there was a very dry year in the
Sacramento Valley
, photo =Sacramento Riverfront.jpg
, photo_caption= Sacramento
, map_image=Map california central valley.jpg
, map_caption= The Central Valley of California
, location = California, United States
, coordinates =
, boundaries = Sierra Nevada (ea ...
. A man by the name of Rice and some neighbors brought horses and mules up to Rice Valley, and used it and adjoining territory for the fine pasture. Rice Valley was their headquarters. Rice was active in that area for only a few years, but Rice Valley, Rice Creek, and the Rice Fork took his name.
At one time, an Indian trail went from the hot springs down the Rice Fork canyon to the mouth of the river where it entered
Gravelly Valley
Hullville (also, Gravelly Valley) is a former settlement in Lake County, California. Hullville was located east-southeast of Bear Mountain. It was inundated by Lake Pillsbury
Lake Pillsbury is a lake in the Mendocino National Forest of Lake C ...
, then crossed the river at the upper end of the valley, then went up Squaw Valley Creek to the north of Big Squaw Valley and over the ridge to the Indian village at Bloody Rock. A portion of this trail is now under Lake Pillsbury.
Watershed
Snow Mountain There are various mountains called Snow Mountain in the United States:
See also
* Snow Mountain Wilderness, California
* Mount Snow, Vermont, United States
* Snow Peak (disambiguation)
* Ice Mountain (disa ...
-West at dominates the landscape on the east side of the Rice Fork
watershed. Its massive west ridge drops down to Lake Pillsbury and divides the Rice Fork from the Eel River watershed, and its southern ridge connects with Goat Mountain about southeasterly to separate Rice Fork from the South Fork Stony Creek (Sacramento River) waters.
To the west of Snow Mountain-West, the ridges of Pine Mountain, Horse Mountain, and
Elk Mountain Elk Mountain may refer to:
Settlements
* Elk Mountain, Utah, a settlement in the U.S. state of Utah
* Elk Mountain, Wyoming, a settlement in the U.S. state of Wyoming
Summits
*Elk Mountain (British Columbia), a mountain in British Columbia, Canad ...
connect to form the western boundary of Rice Fork's watershed, while French Ridge joins with Little Horse Mountain and the west ridge of Goat Mountain to define the southern limit, with all the waters flowing into Lake Pillsbury, the Eel River and on to the
Pacific Ocean
The Pacific Ocean is the largest and deepest of Earth's five oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean (or, depending on definition, to Antarctica) in the south, and is bounded by the contine ...
.
The average slope of Rice Fork is , and between and elevation. The Rice Fork drains 33 percent of the total drainage area of Lake Pillsbury, and may contribute a like percentage of the amount of inflow. The Rice Fork arm contains 7 percent of the surface area and 6 percent of the total volume of the reservoir. Most of the
sediment
Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sa ...
in Lake Pillsbury is deposited in the upper reaches of the Eel River and Rice Fork arms.
Hale Ridge Research Natural Area (RNA)
Rice Fork defines the southern boundary of the Hale Ridge Research Natural Area (RNA), and parallels the east side of Forest Road 17N04 (Twin Valley Road), as it flows along the western boundary of the RNA for about one mile. A designated
critical habitat
Critical habitat is a habitat area essential to the conservation of a listed species, though the area need not actually be occupied by the species at the time it is designated. This is a specific term and designation within the U.S. Endangered Sp ...
for the federally protected
northern spotted owl
The northern spotted owl (''Strix occidentalis caurina'') is one of three spotted owl subspecies. A western North American bird in the family Strigidae, genus '' Strix'', it is a medium-sized dark brown owl native to the Pacific Northwest
...
, and a winter range for
black-tailed deer
Two forms of black-tailed deer or blacktail deer that occupy coastal woodlands in the Pacific Northwest of North America are subspecies of the mule deer (''Odocoileus hemionus''). They have sometimes been treated as a species, but virtually all ...
, the RNA was established by the
U.S. Forest Service
The United States Forest Service (USFS) is an agency of the United States Department of Agriculture, U.S. Department of Agriculture that administers the nation's 154 United States National Forest, national forests and 20 United States Nationa ...
in 1987 to represent the
knobcone pine
The knobcone pine, ''Pinus attenuata'' (also called ''Pinus tuberculata''), is a tree that grows in mild climates on poor soils. It ranges from the mountains of southern Oregon to Baja California with the greatest concentration in northern Calif ...
forest for the
North Coast Ranges. Within the RNA, dense stands of knobcone pine and mixed conifer forest, dominated by
Douglas-fir
The Douglas fir (''Pseudotsuga menziesii'') is an evergreen conifer species in the pine family, Pinaceae. It is native to western North America and is also known as Douglas-fir, Douglas spruce, Oregon pine, and Columbian pine. There are three ...
, also provides a dispersal habitat for a Forest Service-listed sensitive species, the
northern goshawk
The northern goshawk (; ''Accipiter gentilis'') is a species of medium-large raptor in the family Accipitridae, a family which also includes other extant diurnal raptors, such as eagles, buzzards and harriers. As a species in the genus '' Acci ...
.
The underlying rocks of the RNA are all
greywacke
Greywacke or graywacke ( German ''grauwacke'', signifying a grey, earthy rock) is a variety of sandstone generally characterized by its hardness, dark color, and poorly sorted angular grains of quartz, feldspar, and small rock fragments or li ...
sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks.
Most sandstone is composed of quartz or feldspar (both silicates ...
s and
shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especia ...
s. The greywacke has a muddy, brownish-gray sandstone appearance, ranging from rather soft and crumbly in weathered outcrops to solid rocks and boulders in the stream bed of the Rice Fork.
Some recreationists use Crabtree Hot Springs which is adjacent to the northwestern boundary of the RNA. The Rice Fork is also lightly used for recreation, but entry into the RNA is minimal. There is an unknown increase in risk of wildfire due to human use at the hot springs.
Tributaries
Salt Creek is one of the larger tributaries, and flows from Fir Root Spring. Beginning at about above sea level, on the west slope of Goat Mountain's northwest ridge, it travels southwesterly down a steep canyon for about , going over a falls and crossing a forest road, entering Rice Fork on the right at around , about upstream from the lake, and around a quarter mile upstream from Crabtree Hot Springs.
French Creek begins at about above sea level near the top of French Ridge, and flows north down a steep canyon for about , adding its tributary, entering Rice Fork on the left at around , about upstream from the lake, and about a mile downstream from Crabtree Hot Springs. Rock Creek (tributary to French Creek) begins at about on Elk Mountain and flows northeasterly for about down a steep canyon, entering French Creek on the left about upstream from its confluence with Rice Fork.
Soda Creek begins at about on Elk Mountain and flows east down a steep canyon, entering Rice Fork on the left a short distance upstream from Parramore Creek, as indicated on the
USFS
The United States Forest Service (USFS) is an agency of the U.S. Department of Agriculture that administers the nation's 154 national forests and 20 national grasslands. The Forest Service manages of land. Major divisions of the agency inc ...
2008 map.
Parramore Creek begins at about on Elk Mountain and flows east for about down a steep canyon, crossing a forest road at Three Crossings, entering Rice Fork on the left about upstream from the lake.
Bear Creek flows from a spring at about on the southwest side of Snow Mountain-West. It drops rapidly down a steep canyon and flows southwesterly for about , adding its tributary, passing underneath a
concrete
Concrete is a composite material composed of fine and coarse aggregate bonded together with a fluid cement (cement paste) that hardens (cures) over time. Concrete is the second-most-used substance in the world after water, and is the most ...
bridge and crossing a forest road, entering Rice Fork on the right about upstream from the lake. Blue Slides Creek (tributary to Bear Creek) begins at about , on the west slope of Goat Mountain's northwest ridge, and flows west for about down a steep canyon, finally paralleling the south side of Forest Road M-10 (county road 301-C), as it enters Bear Creek on the left just after the bridge.
Bevans Creek begins at about above sea level on Horse Mountain and flows northeasterly for about down a steep canyon, entering Rice Fork on the left about upstream from the lake.
Rice Creek begins at about on the west ridge of Snow Mountain-West. It swiftly descends the steep west slope of the mountain, flowing southwesterly for about down a steep canyon, crossing a forest road and passing through Rice Valley, entering Rice Fork on the right about upstream from the lake.
Deer Creek begins at about on the west ridge of Snow Mountain-West, and flows west for about down a steep canyon, crossing a forest road, entering Rice Fork on the right about upstream from the lake.
Willow Creek begins at about on Horse Mountain and flows northeasterly for about down a steep canyon, entering Rice Fork on the left about upstream from the lake.
Packsaddle Creek begins at about on Pine Mountain and flows northeasterly for about down a steep canyon, entering Rice Fork on the left near Swallow Rock, at the southern tip of the lake.
River crossings, campgrounds and trailheads
River and creek crossings
*Forest Road 17N04 (Twin Valley Road) crosses both Rice Fork and Salt Creek at their confluence.
*Forest Road M-10 (county road 301-C) crosses Rice Fork a short distance downstream from its confluence with Bear Creek.
*Forest Road M-10 (county road 301-C) bridges Bear Creek at its confluence with Blue Slides Creek.
*Forest Road M-3 (18N04) crosses Rice Creek about 2 miles north of its junction with Forest Road M-10 (county road 301-C).
*Forest Road M-3 (18N04) crosses Deer Creek about 5 miles north of its junction with Forest Road M-10 (county road 301-C).
*Forest Road 17N16 (Long Ridge Road) crosses Bear Creek at its junction with Forest Road M-10 (county road 301-C).
Campgrounds and trailheads
*Bear Creek Campground (USFS) – Free & open all year, maximum stay 14 days, 16 picnic tables & grilles + 2 toilets, elevation . Set beside Bear Creek near its confluence with Blue Slides Creek, on Forest Road M-10 (county road 301-C) about northeast from its junction with Elk Mountain Road. This is the only public campground in the Rice Fork Eel River watershed.
*Summit Springs Trailhead is located at about on the south ridge of Snow Mountain-West. A hiking trail follows the ridge line to the top of Snow Mountain West Peak and East Peak. Forest Road M-10 (county road 301-C) crosses the south ridge at about . A secondary forest road continues up the ridge to the trailhead.
See also
*
Rivers of Lake County, California
Rivers and creeks in Lake County, California are listed below by river basin and alphabetically.
Unless otherwise stated, the information is taken from the Geographic Names Information System maintained by the United States Geological Survey.
Co ...
References
Mauldin's Notes on Lake County HistorySignature Page for Research Natural Area Establishment Record, Hale Ridge Research Natural Area, Mendocino National Forest, Lake County, California - 1987USFS Mendocino National ForestCurrent Stream Habitat Distribution Table - NOAA 1993*USGS POTATO HILL Quadrangle, California, 7.5-minute series topographic - 1996
*USGS FOUTS SPRINGS Quadranglle, California, 7.5 minute series topographic - 1996
*DFG Department of Fish and Game. 1993a. Rice Fork Eel River Stream Survey, August 16–19, Report by Kyle Murphy, Twyla Anderson, and Carl D. Reese
*DFG Department of Fish and Game. 1993b. Packsaddle Creek Stream Survey, August 19, Report by Albert Rodriguez and Andrew Boydstun
*DFG Department of Fish and Game. 1993c. Willow Creek Stream Survey, August 19, Report by Will Abel and Kerry Padgett
*DFG Department of Fish and Game. 1993d. Deer Creek Stream Survey, August. Report by Carl D. Reese, Albert Rodriguez, and Jim Murphy
*DFG Department of Fish and Game. 1993e. Rice Creek Stream Survey, August 16, Report by Kerry Padgett and Weldon E. Jones
*DFG Department of Fish and Game. 1993g. Bevans Creek Stream Survey, September 24, Report by Alice Berg, Carl D. Reese, and Kerry Padgett
*DFG Department of Fish and Game. 1993h. Bear Creek Stream Survey, August 16, 18, 31, Report by Carl D. Reese, Carl Murphy, and Kerry Padgett
*DFG Department of Fish and Game. 1993j. Parramore Creek Stream Survey, August 18, Report by Alvert Rodriguez and Andrew Boydstun
*DFG Department of Fish and Game. 1993k. French Creek Stream Survey, August 11, Report Carl D. Reese and Carl Murphy
*DFG Department of Fish and Game. 1993m. Salt Creek Stream Survey, August 17, Report by Albert Rodriguez and Andrew Boydstun
*USFS United States Forest Service. 2006b. French Creek Observations 2006, Lee Morgan Forest Fish Bio.
*Geological Survey Water-Supply Paper 1619-EE, Sedimentation of Lake Pillsbury, Lake County, California, United States Department of the Interior, Stewart L. Udall, Secretary, U.S. Government Printing Office, Washington 1964
External links
Photographic Journey - Friends of the Eel River
{{Eel River
Rivers of Lake County, California
Hot springs of California
Rivers of Northern California
Tributaries of the Eel River (California)