National marine sanctuary offices and visitor centers closed to the public; waters remain open

NOAA's national marine sanctuary offices and visitor centers are closed to the public while the waters remain open for responsible use in accordance with CDC guidance and local regulations. More information on the response from NOAA's Office of National Marine Sanctuaries can be found on

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Because central California is a tectonically active area with extensive coastal uplift, coastal erosion rates are high. Erosion rates vary along the MBNMS coast, depending on the coastal morphology, lithologies and degree of rock fragmentation (i.e. faulting and jointing). Along the northern and north central segments, erosion rates are moderate to high (long term rates of about 30 cm/yr) due to the exposure of fairly erodable Tertiary sedimentary rocks. However, erosion near Capitola, where the Purisima Formation is located in the surf zone, has been recorded as high as 1.5 m/yr (Plant and Griggs 1991).

Along the south central and southern MBNMS segments, coastal erosion is slower due to the resistant nature of coastal rocks. Exposed granitic basement and well lithofied Cretaceous sedimentary rocks withstand wave attack better than the more northerly coastal cliffs. However, erosion rates are higher in locations where Franciscan rocks are exposed and granitic rocks are highly fractured from faulting. Point Sur stands out as a resistant gabbro body within the more erodable Franciscan mass. Unfortunately, no good erosion rates exist for this part of the MBNMS.

Although coastal erosion is a continuous process, the rate of erosion is accelerated during times of severe storm activity (Griggs and Johnson 1979, 1983). In addition, human-made structures placed in the coastal zone have increased erosion locally (Plant and Griggs 1991; also see Coastal Dunes section).

Much of the eroded materials are transported along the coast to canyon heads where they are lost to the sedimentary system. Material transport can be seen as coarse sand bands on the continental shelf (Arnal et al. 1973, Chin 1984, Chin et al. 1988, Hunter et al. 1988, Yancy 1968). Much of this transported material travels down canyons as turbidity currents, especially during earthquakes (Garfield et al. 1994). These sediments are deposited as overbank features and sand waves at the base of the continental slope (Normark et al. 1980).

Numerous major rivers and streams also carry considerable eroded products to the sea; these are eventually deposited on the MBNMS seafloor. In addition to natural eroded detritus, anthropogenic material and waste products are transported through these drainages, and often end up concentrating along the MBNMS coast and the nearshore seafloor. Some may be carried down canyons via mass wasting events, and may ultimately rest on the abyssal plain.

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Section V. Cold Seeps