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THE STRATA PLAZA AS A TEACHING TOOL
The concrete
colors, textures, embedded rocks and fossils were specifically designed
to represent the rock layers seen around San Diego.
Students can learn
about the natural history of San Diego and the geologic record as seen
in local sedimentary strata.
- The Mesozoic Peninsula Range Plutonic Igneous Rocks crystallized
deep below a volcanic mountain range associated with an ancient
subduction zone.
- The Cretaceous Santiago Peak Volcanics erupted from volcanoes
formed over an ancient subduction zone.
- The Cretaceous Point Loma Formation
outcrops along the beach cliffs in Point Loma and La Jolla Cove. It
formed from turbidity currents flowing down a submarine canyon and contains
many fossils including snails, clams, ammonites, and worm burrows.
- The Cretaceous
Cabrillo Formation formed on an offshore Submarine fan.
- The Eocene Mt.
Soledad Formation is the oldest in a thick section of Eocene sediments
found in San Diego . It can be distinguished from the Cretaceous Cabrillo
Formation by the presence of distinctive purple-pink clasts.
- The Eocene
Delmar Formation, which was deposited in a coastal lagoon, outcrops
on the beach cliffs at Torrey Pines State Park.
- The Eocene Torrey Sandstone,
which outcrops on the beach cliffs at Torrey Pines State Park was
deposited along a coastal beach or tidal flat.
- The Eocene Ardath Shale was deposited
underwater, and is characterized by thin bedding.
- The Eocene Scripps Formation,
which outcrops at Tourmaline Beach Surfing Park , was deposited underwater.
- The Eocene Poway Group, contains several formations, like the Stadium
Conglomerate, which outcrops on the cliffs along Friars Road near the
Stadium.
- The Pliocene
San Diego Formation was deposited when a bay covered San Diego . It
is rich in many types of fossils including marine mammals and sharks.
- The Pleistocene
Linda Vista Formation, which can be seen atop many of the mesas in
San Diego was deposited during the Ice Ages and is characterized by a
distinctive rust-red color.
- The Pleistocene Crown Point Formation, which outcrops
near Crown Point , was deposited in a bay or estuary during an interglacial
period of high sea level between the Ice Ages.
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