GeologyWhile the island is not a volcano it is composed primarily of Miocene volcanic rocks (basalt) interbedded with marine sediments.2 The steep wave-cut cliffs of its shoreline indicate that this is one of the younger Channel Islands. It exhibits at least six marine terraces; evidence of repeated tectonic uplift and subsidence (so called porpoising). Arch Point, on the north-east shore of the island is a 130 ft (40 m) arch causd by wave erosion of fault weakened rock.3 Offshore, there are two named rocks: Shag Rock off the northerly shore (1 acre) and Sutil Island off the southwest end (12 acres). HistoryThe first European visitor to the Channel Islands in 1542, Juan Rodriguez Cabrillo, a Portuguese explorer, made no mention of this island. Sixty years later, the island was named by Spanish explorer Sebastian Vizcaino, who visited the island on December 4, 1602, the feast day dedicated to Santa Barbara. In December 1934, the factory ship California spent a week anchored off Santa Barbara Island, processing whales caught by her two steam-driven whale catchers.4 WildlifeSanta Barbara Island is home to a large sea lion rookery and seabird nesting colonies. It is also home to the largest breeding colony for Xantus's Murrelet, a threatened seabird species. Xantus's murrelet is listed as vulnurable, because so much of their breeding takes place on such a small and isolated island. Santa Barbara Island live-forever (Dudleya traskiae) is a succulent plant endemic to the island. References
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