This week I went to Santa Catalina Island to explore its
complex and interesting geology. Santa Catalina Island is one of the channel
islands of the California archipelago.
The island looks like an interesting mix of Cretaceous and Jurassic sandstone, Tertiary volcanic rocks
with minor pyroclastic deposits, a great variety of pre-Cenozoic
metasedimentary and metavolcanic rocks with small pockets of ultramafic rocks
(mostly serpentine), and one small section of Miocene marine sandstone on the
south eastern tip of the island.
To learn more about the island’s geology I would request:
1.
The rock that makes up Catalina Island
appears to be very young but also varied. What processes occurred to create the
island?
2.
This
partially ties in with my first request, how does this small island have such a
varied makeup? On the eastern end of the island, it is primarily Precambrian
granite, on the western end it is primarily Mesozoic sandstone and portions of
the middle are Tertiary volcanic rocks.
3.
Is there evidence of the island being created
or partially created as part of a fold? It seems odd to me that the “KJf” rock
(KJf = Cretaceous and Jurassic sandstone of the Franciscan Complex) is both on
the western side and eastern side of the island.
References
Geologic Map of California (2010). (2010). Retrieved from https://maps.conservation.ca.gov/cgs/gmc/
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