Goat Rock Beach | |
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Coordinates: 38°26′48″N123°7′35″W / 38.44667°N 123.12639°W | |
Location | Sonoma County, California |
Part of | Sonoma Coast State Beach |
Offshore water bodies | Russian River (California) |
Operator | State of California |
Goat Rock Beach is a sand beach in northwestern Sonoma County, California, United States. This landform is a sub-unit of Sonoma Coast State Beach, owned and managed by the State of California. At the northern terminus of Goat Rock Beach is the mouth of the Russian River, and the southern end of this crescent shaped expanse is the massive Goat Rock, an iconic outcrop of the Sonoma Coast, which is barely attached to the mainland by a narrow isthmus.
Goat Rock Beach is frequented by beachcombing visitors, but usually not in high numbers, except in mid-summer; there is some wading and surfing activity, although these uses are moderated by the rip current generated by a steep gradient into the water that leads to an underwater trench parallel to the waterline. The beach is also a regular resting ground for a variety of gulls (including Western Gull, California Gull, and Ring Billed Gull), river otters, elephant seals, harbor seals, and sea lions, with the latter three species often hauling out of the Pacific Ocean. The state of California recommends that a 50-yard (46 m) distance be preserved between human visitors and the seasonal marine mammals, especially in the pupping season.
The Russian River, with its mouth at the north end of Goat Rock Beach, is Sonoma County's largest watercourse, both in flow rate and lineal extent. Immediately beyond the Russian River discharge to the Pacific Ocean is the coastal town of Jenner. North of the mouth of the Russian River is Jenner Beach. Goat Rock protrudes into the Pacific at the south end of Goat Rock Beach. Visitors can access the base of Goat Rock via a low lying isthmus of land which has been appropriated by the State as a parking area. The almost sheer cliffs of Goat Rock are virtually impossible to scale or to circumnavigate; in fact, signage is posted prohibiting either activity. There is considerable sloughing of broken rock from these vertical surfaces of Goat Rock. Blind Beach is situated immediately south of Goat Rock Beach, the two beaches being separated by Goat Rock itself.
Along Goat Rock Beach and the adjoining beaches, massive rock outcroppings are found both on the shore and protruding from the Pacific Ocean as small skerries. Among these rugged structures are natural arches formed by powerful wave action selectively eroding weaker strata of the rock formations. Approximately 17 mi (27 km) to the south is another major geological feature of the Northern California coast known as Bodega Head. Goat Beach lies below and slightly west of State Route 1.
During the summer months, a sandbar is built up along the beach and separates the Russian River from the Pacific Ocean. This sandbar is breached whenever the water levels reach heights between 4.5–7 feet (1.4–2.1 m) at the Jenner visitor center. [1] Breaching of the sandbar during late fall/early winter splits the beach in two sections. The northern section is protected by the Russian River flowing into the ocean and creates an ideal location for harbor seal pupping.
The Russian River State Marine Reserve and Russian River State Marine Conservation Area protect the Russian River Estuary. Like underwater parks, these marine protected areas help conserve ocean and freshwater wildlife and marine ecosystems.
Goat Rock Beach is subject to continuing marine erosion as well as windborne erosion, thus creating a situation where an average of 1 to 3 ft (0.30 to 0.91 m) per year of land mass is lost, [2] except for the hardest of outcrop formations. In winters of heavy storms, this value can be yet higher. Over the last geologic epoch the land has been subject to uplift, [2] a process combined with marine erosion, which has created a marine terrace above the entire extent of the beach. This marine terrace elevation varies approximately 30–150 feet (9.1–45.7 m) above mean sea level, which results in a steep bluff directly above the littoral zone, and a succession of terrace levels.
The sea stacks along the coast at Goat Rock Beach consist of rocks from the Franciscan Complex, formed within an era of plate collision along the western coast of North America. From about 200 to 30 million years ago, the North American Plate was in continual collision with the Farallon Plate. [3] A variety of rock types resulted from this collision, including pillow basalt, chert, and marine sandstone. During the plate collisions, these rocks were considerably faulted and crushed into melange, which is a mixture of ground-up matrix and resistant pockets of rock floating within. When melange is eroded by wave action, the softer part of the matrix is washed away, leaving the more resistant blocks exposed in the ocean as sea stacks. Goat Rock is such a flat topped [4] sea stack consisting of a block of resistant greywacke.
Vertical sea stack formations, a geological hallmark of this shoreline, appear standing out of the water or on the beach resembling sculptures. Occasionally these stacks appear on the marine terrace, indicating their ancient genesis on the sea floor prior to uplift. These rock formations are characteristically composed of sandstone with layers of quartz.
The active San Andreas Fault runs roughly parallel and near to the coastline of Goat Rock Beach. Soils within the site are classified as coastal beach sands (where rocky shoreline is not evident) and escarpment group soils on the marine terrace; typically soils above the marine terrace are in the Rohnerville loam group. [5] Most of the beach sands consist of a medium coarse brown to gray sandy materials, reflecting the high rate of erosion of escarpment soils into the ocean; however, there are patches of dark gray smooth pebble beach such as the approximately 100 metres (328 ft) stretch lying immediately north of Goat Rock. The beach is changed every year.
The oldest natural history of this area related to mammals manifests in a series of rock outcrops about one third of a mile south of Goat Rock Beach, positioned above the shoreline on a low lying marine terrace. There are uplifted sea stack formations with prominent rubbing marks about 2 to 4 metres (6 ft 7 in to 13 ft 1 in) in elevation above the ground surface, a height too high to have been caused by modern bovids. Mammoths are believed to have roamed here as recently as 40,000 years ago, and they are thought to have created these severe rubbing marks. [6] Mammoth fossil remains have been found at Bodega Head at the south end of Sonoma Coast State Beach.
The earliest known human settlement of this site was by the Native American Coast Miwok and Pomo tribes. As early as 1849 archaeological discoveries were recorded in the vicinity, and to date several prehistoric kitchen middens and other types of tribal habitation finds have been made. Goat Rock Beach is part of the Mexican land grant rancho Bodega. [7] The Russians are thought to have begun logging the old-growth forests directly above the coastal prairie in the early 19th century.
The underwater delineation of the property is considered to extend to 1,000 feet (305 m) from the shoreline. While no shipwrecks have been discovered, the literature indicates that there are at least 17 vessels which may have been lost in these waters. There are remains of numerous historic barns and other agricultural buildings on the coastal prairie several miles south of Goat Rock Beach, indicating 19th century settlement by Europeans; to the south, at Duncans Landing there are iron pins embedded in the sandstone bluffs as evidence of an active shipping industry here in the late 19th and early 20th century.
In the era circa 1920, a sizeable quarrying was conducted at Goat Rock, which activity produced the apparent separation of Goat Rock from the mainland. Quarry products were transported to the mouth of the Russian River via a now abandoned rail line; some of these materials were used to attempt the construction of a jetty in the mouth area, but that project was eventually terminated.
There are three distinct habitats present at Goat Rock Beach, including marine, littoral zone and coastal prairie. The marine environment presents gray whales, harbor seals, [8] and California sea lions, as well as a multitude of fish species and other marine organisms; in fact, several species of anadromous fish enter the Russian River estuary and migrate for tens of miles up the Laguna de Santa Rosa and other Russian River tributaries. [9] Furthermore, a variety of pelagic birds and shorebirds are locally in evidence. Additionally, there are modest kelp beds and other marine vegetation. The littoral beach environment has fewer organisms than more southerly zones of California, because of the colder temperatures here.
The coastal prairie soils on the marine terrace above the beach are moderately well drained and granular with moderate soil permeability; these features manifest high erosion potential and moderately high bio-productivity. Acidity of these loamy soils is medium to high, and thus some vegetative stunting and hospitality to rare plants is offered; however, the tree stunting is not as pronounced as farther north along the Mendocino coast, which presents extensive and exaggerated pygmy forests. The upland environment on the coastal prairie offers a range of grass species and wildflowers including varieties of lupine, thistle and wild oats. The typical annual plant productivity is approximately 1,500 kilograms (3,307 lb) per acre of air dried yield per annum in an abundant moisture year, and about half that amount in a very dry year. A variety of birds and mammals thrive on the coastal prairie including numerous California Mule Deer, Odocoileus hemionus californicus.
Due to the potential safety risks of strong rip currents and sneaker waves at Goat Rock Beach, swimming is strictly prohibited. There are restroom facilities, a parking lot, and picnic tables on site. [10] Hang-gliding is permitted from a 150 feet (46 m) high launch point on a high marine terrace above the southern part of Goat Rock Beach, provided the participant is in possession of USHGA card, Sonoma Wings card, and signed waiver card. [11]
A coast – also called the coastline, shoreline, or seashore – is the land next to the sea or the line that forms the boundary between the land and the ocean or a lake. Coasts are influenced by the topography of the surrounding landscape, as well as by water induced erosion, such as waves. The geological composition of rock and soil dictates the type of shore that is created. Earth contains roughly 620,000 km (390,000 mi) of coastline.
Coastal erosion is the loss or displacement of land, or the long-term removal of sediment and rocks along the coastline due to the action of waves, currents, tides, wind-driven water, waterborne ice, or other impacts of storms. The landward retreat of the shoreline can be measured and described over a temporal scale of tides, seasons, and other short-term cyclic processes. Coastal erosion may be caused by hydraulic action, abrasion, impact and corrosion by wind and water, and other forces, natural or unnatural.
Landforms are categorized by characteristic physical attributes such as their creating process, shape, elevation, slope, orientation, rock exposure, and soil type.
A raised beach, coastal terrace, or perched coastline is a relatively flat, horizontal or gently inclined surface of marine origin, mostly an old abrasion platform which has been lifted out of the sphere of wave activity. Thus, it lies above or under the current sea level, depending on the time of its formation. It is bounded by a steeper ascending slope on the landward side and a steeper descending slope on the seaward side. Due to its generally flat shape, it is often used for anthropogenic structures such as settlements and infrastructure.
Coastal management is defence against flooding and erosion, and techniques that stop erosion to claim lands. Protection against rising sea levels in the 21st century is crucial, as sea level rise accelerates due to climate change. Changes in sea level damage beaches and coastal systems are expected to rise at an increasing rate, causing coastal sediments to be disturbed by tidal energy.
In geology, a terrace is a step-like landform. A terrace consists of a flat or gently sloping geomorphic surface, called a tread, that is typically bounded on one side by a steeper ascending slope, which is called a "riser" or "scarp". The tread and the steeper descending slope together constitute the terrace. Terraces can also consist of a tread bounded on all sides by a descending riser or scarp. A narrow terrace is often called a bench.
Mussel Rock is a rock formation on the coast of San Mateo County, California, offshore from Daly City. It consists of one large and numerous smaller rocks of a type known as a stack, where a headland is eroded unevenly, leaving small islands. The rock itself is located 15 meters from the shore of Mussel Rock Park and stands 18 meters tall.
Fowlsheugh is a coastal nature reserve in Kincardineshire, northeast Scotland, known for its 70-metre-high (230 ft) cliff formations and habitat supporting prolific seabird nesting colonies. Designated as a Site of Special Scientific Interest (SSSI) by Scottish Natural Heritage, the property is owned by the Royal Society for the Protection of Birds. Fowlsheugh can be accessed by a public clifftop trail, or by boats which usually emanate from the nearby harbour at the town of Stonehaven. Tens of thousands of pelagic birds return to the site every spring to breed, after wintering at sea or in more southern climates, principal species being puffins, razorbills, kittiwakes, fulmars and guillemots.
The Russian River is a southward-flowing river that drains 1,485 sq mi (3,850 km2) of Sonoma and Mendocino counties in Northern California. With an annual average discharge of approximately 1,600,000 acre feet (2.0 km3), it is the second-largest river flowing through the nine-county Greater San Francisco Bay Area, with a mainstem 115 mi (185 km) long.
Sonoma Coast State Park is a State of California property in Sonoma County consisting of public access use on lands adjoining the Pacific Ocean. This extent of beach runs from a coastal point about 4 miles (6 km) north of Jenner and continues for approximately 17 miles (27 km) to the south to terminate at Bodega Head. The property lies along State Route 1 and consists of a number of named beaches including Arched Rock Beach, Gleason Beach and Goat Rock Beach. The ecosystem consists of alternating sandy beaches and rocky shoreline, with a marine terrace extending above the entire extent with an upland California coastal prairie habitat.
Salt Point State Park is a state park in Sonoma County, California, United States. The park covers 6,000 acres (2,428 ha) on the coast of Northern California, with 20 miles (32 km) of hiking trails and over 6 miles (9.7 km) of a rough rocky coastline including Salt Point which protrudes into the Pacific Ocean. The park also features the first underwater preserves in California. The constant impact of the waves forms the rocks into many different shapes. These rocks continue underwater providing a wide variety of habitats for marine organisms. The activities at Salt Point include hiking, camping, fishing, scuba diving and many others. The weather is often cool with fog and cold winds, even during the summer.
Beach evolution occurs at the shoreline where sea, lake or river water is eroding the land. Beaches exist where sand accumulated from centuries-old, recurrent processes that erode rocky and sedimentary material into sand deposits. River deltas deposit silt from upriver, accreting at the river's outlet to extend lake or ocean shorelines. Catastrophic events such as tsunamis, hurricanes, and storm surges accelerate beach erosion.
Duncans Point is a cape on the Pacific Coast of northern California in the United States. It is located in Sonoma County at 38.393°N 123.0947°W, approximately 45 miles (70 km) northwest of San Francisco and approximately 20 miles (30 km) west of Santa Rosa.
Doran Regional Park is a regional park south of Bodega Bay, California, U.S.A. that is maintained by the Sonoma County Regional Parks Department. It covers an area of 127 acres (51 ha). It is located at 38.314°N 123.0428°W on the sand spit separating Bodega Harbor from Bodega Bay. The park address is 201 Doran Beach Road, Bodega Bay, CA.
Coastal engineering is a branch of civil engineering concerned with the specific demands posed by constructing at or near the coast, as well as the development of the coast itself.
The Coast Range ecoregion is a Level III ecoregion designated by the Environmental Protection Agency (EPA) in the U.S. states of Washington, Oregon, and California. It stretches along the Pacific Coast from the tip of the Olympic Peninsula in the north to the San Francisco Bay in the south, including Grays Harbor, Willapa Bay, and the Long Beach Peninsula in Washington, the entire length of the Oregon Coast, and the Northern California Coast. Named for the Coast Range mountains, it encompasses the lower elevations of the Olympic Mountains, the Oregon Coast Range, the Californian North Coast Ranges, and surrounding lowlands.
Bodega Head State Marine Reserve (SMR) and Bodega Head State Marine Conservation Area (SMCA) are two adjoining marine protected areas off Bodega Bay in Sonoma County on California’s north-central coast. The combined area of these marine protected areas is 21.64 square miles (56.0 km2), with 9.3 square miles (24 km2) in the SMR, and 12.34 square miles (32.0 km2) in the SMCA. Bodega Head SMR prohibits the take of all living marine resources. Bodega Head SMCA prohibits the take of all living marine resources, except the recreational and commercial take of pelagic finfish with troll fishing gear or seine, Dungeness crab by trap, and market squid by hand-held dip net and round haul net.
Russian River State Marine Recreational Management Area (SMRMA) and Russian River State Marine Conservation Area (SMCA) are two adjoining marine protected areas in the Russian River estuary area in Sonoma County, California, on the north-central coast of the state. The combined area of these marine protected areas is 1.21 square miles (3.1 km2), with 0.35 square miles (0.91 km2) in the SMRMA and 0.86 square miles (2.2 km2) in the SMCA.
Cape Town lies at the south-western corner of the continent of Africa. It is bounded to the south and west by the Atlantic Ocean, and to the north and east by various other municipalities in the Western Cape province of South Africa.