Introduction
The
proposed Chumash Heritage National Marine Sanctuary (CHNMS) is located
along the pristine south Central California coastline, from Gaviota
Creek to the south to Santa Rosa Creek in Cambria to the north. The
western boundary of the CHNMS would be west of the submerged Santa
Lucia Bank along the Santa Lucia Escarpment. The eastern boundary would
be the mean high tide line along the coastline. These pristine coastal
waters are between the Channel Islands National Marine Sanctuary
(CINMS) and the Monterey Bay National Marine Sanctuary (MBNMS). There
are seven nationally and internationally important core areas within
this proposed sanctuary that were originally identified in the 1990
proposal to become the Central Coast National Marine Sanctuary;
however, the proposal died because of Congressional inaction.
Seven
Core Areas
Detailed
maps of the core areas can be found in the April
2014 SLO Coast Journal
and on the Chumash
Sanctuary website.
Core Area One is the nearshore area from mean high tide line out 3 to
13 miles offshore of this proposed sanctuary coastline. This area
contains many of the submerged Cultural Chumash Sacred Sites ranging
from villages to possible solstice alignments. Chumash records suggest
occupation of the central coast area for more than 15,000 years with an
older recorded date at Point Conception, an extremely important Chumash
Sacred Place known to Native Americans as the Western Gate. Other sites
adjacent to or extending into submerged land include: Jalama; two
10,000 year- old sites within Vandenberg AFB; sites at Point Sal; four
major Chumash Sacred sites onshore San Luis Bay of which three are
known to have been continuously occupied for at least 9,000 years: the
site for which the City of Pismo Beach is named, the site where the
Chumash people return to renew the Traditional Ritual Ceremony Cycle,
the old Chumash Capital in the area of Avila Beach, now partially
covered by sea level rise; the Chumash Sacred site at Diablo Cove along
the coastline of the Pecho Coast dated over 9,000 years; the Chumash
Village Sacred site in Los Osos; hundreds of Chumash Sacred sites
ringing Morro Bay; the Chumash village Sacred site of Cayucos
(continuously occupied for 8,000 years); other large sites found in the
area to a mile north of Pt. Estero; and two Chumash village Sacred
sites in Cambria continuously occupied for 10,000 years.
Core
Area Two is located off the California Central Coast between the
Channel Islands and Monterey Bay National Marine Sanctuaries. Within
its boundaries are an upthrust block, a mile deep sea canyon, and a
seamount. The Santa Lucia Bank upthrust block rises to within 400
meters of the ocean surface 30 to 40 miles offshore from the north face
of the Arguello Canyon to offshore Morro Bay. This area lies within the
Oceanographic and Meteorological transition zone of the Oregonian and
Californian Providences at the complex meeting place of south and north
moving major warm and cold ocean currents.
The
complex topography is the result of the meeting place of three major
tectonic plates. Topography within the boundary — the
Rodriquez Seamount, the Arguello Canyon, Santa Lucia Bank and the Santa
Lucia Escarpment — and adjacent topography to its south area
outside the boundary line — the Southern California Bite and
the Channel Islands — enhances a meeting place of these major
ocean currents that guides and funnels the West Coast’s only
persistent upwelling that rises between Points Arguello and Sal feeding
whales and birds throughout the Pacific.
Core
Area Three is from Gaviota Creek, south of Point Conception, to
Purisima Point. This area contains thriving kelp forests, wetlands,
Kashtayit State Marine Conservation Area, two state Marine Protection
Areas (MPA), historic major shipwrecks, and onshore Gaviota State Park
and Jalama Beach County Park. The richness of the marine habitat is
dependent upon the adjacent permanent upwelling waters.
Core
Area Four is from Point Sal to Arroyo Grande Creek. This area contains
kelp forests, wetlands, and onshore National Natural Landmark (the
largest California Coastal Dunes Complex), Point Sal State Beach,
Oceano Dunes State Beach, and Pismo State Beach.
Core
Area Five, a rocky intertidal area of northern San Luis Bay, begins at
the northernmost end of the 26-mile stretch of sandy beach called Pismo
Beach. From this rocky cliff area along the coastline to the southern
end of Avila Beach, another high rocky cliff, the boundary arcs
offshore to the 200 meter bathymetric line back to the Pismo Beach
rocky cliffs in order to protect prominent offshore rock habitat in the
San Luis Bay.
Along
this stretch of coast is a major complex of kelp forests; none are
found southward until Point Sal. The coastline varies from rocky cliffs
with no beaches to cliffs with some beach. Despite the beach areas, the
dominant rocky hard bottom offshore provides appropriate habitat for
the kelp forest and its lush populations of plant and animal life. The
area is host to the last significant southernmost population of
southern sea otters in the Southern Sea Otters Range.
This
area is also adjacent to four major onshore Chumash sites -- three
known to have been continuously occupied for 9,000 years. One is the
site for which the city of Pismo Beach was named, one is a site to
which the Chumash have returned to renew the traditional ritual
ceremony cycle, and one is the old Chumash capital in the area of Avila
Beach, now partially covered by sea level rise.
Core
Area Six includes the shoreline of the Pecho Coast, located between
Point San Luis and the Morro Bay Sandspit, the Morro Bay Sandspit to
the north flank of Morro Rock, and the nearshore waters out to the
200-meter bathymetric line.
The
Pecho Coast marine environment consists of a 13-mile stretch of
intertidal rocky reef beginning at Hazard Canyon in the north to Point
San Luis. The shoreline is characterized by sheer, wave-eroded cliffs,
jutting headlands, and massive offshore submerged and exposed rocks.
Above shoreline the narrow coastal bench is flanked by hills. The tidal
zone is generally narrow and may terminate abruptly where protection
from wave shock is minimal and deposition is reduced or absent. These
topographical features form a highly irregular coastline. The coast
provides many different exposed and protected habitats that extend or
control the abundance and composition of marine plants and animals.
This area has 2 state MPAs and is adjacent to the Morro Bay National
Estuary.
Onshore,
are found the oldest known Chumash site on this segment of coastline at
Diablo Cove, a continuously occupied 9,000-year-old Chumash village
site, the Chumash village site in Los Osos, hundreds of Chumash sites
ringing Morro Bay, the sacred site and Bird Refuge of Morro Rock,
Montana de Oro State Park, Point Buchon, and the historic Point San
Luis Lighthouse.
Core
Area Seven is from Cayucos Creek to Santa Rosa Creek. At its northern
end, the Sanctuary would protect the North Estero Bay Intertidal Zone,
extending from the Chumash village site of Cayucos and other large
sites found in the area to a mile north of Pt. Estero. Comprised of
rocky intertidal zones associated with dense kelp forests and other
algae populations, the area supports a wide diversity of life. One of
the largest southern sea otter population clusters resides within this
zone. Offshore rocks provide rookeries and roosting sites for birds and
haulouts for pinnipeds. 500 to 600 harbor seals are found here. Whales
other than gray whales occasionally visit within this zone. Gray whales
stack at Point Estero during migrations. Onshore are found Cayucos
State Beach, White Rock, and Cambria MPAs.
To
summarize, the proposed sanctuary area encompasses submerged Sacred
Chumash sites and possible solstice alignments, historic major
shipwrecks, a Permanent Upwelling, Arguello Canyon, seasonal
upwellings, the Santa Lucia Bank upthrust block, the Rodriguez
Seamount, the Kashtayit State Marine Conservation Area, several
California Department of Fish and Wildlife Marine Protected Areas,
southernmost sea otter cluster, marine mammals and haulouts, wetlands,
rookeries, kelp forests, and other significant nationally and
internationally important marine life and marine ecosystems.
The
unique oceanographic combination of the mile deep canyon, through which
California's and also the West Coast's only persistent upwelling flows,
the Santa Lucia Bank upthrust block, and the Rodriguez Seamount create
the ideal conditions for an internationally and nationally significant
diverse density of marine life attracting whales and birds throughout
the Pacific Ocean to feed at the Santa Lucia Bank.
Onshore
along the coast of the proposed marine sanctuary are
California’s largest coastal dunes complex, Gaviota State
Park, Jalama Beach County Park, Pismo State Beach, Point Sal State
Beach, Oceano Dunes State Beach, Morro Bay National Estuary, Morro Rock
State Landmark and Bird Sanctuary, the historic Point San Luis
lighthouse, Cayucos State Beach. Also, the California Coastal National
Monument includes rocks, islands, exposed reefs, and pinnacles along
the California Coastline.