{"id":5088,"date":"2011-11-14T18:05:56","date_gmt":"2011-11-15T02:05:56","guid":{"rendered":"http:\/\/mlmlblog.wordpress.com\/?p=5088"},"modified":"2011-11-14T18:05:56","modified_gmt":"2011-11-15T02:05:56","slug":"learning-about-the-central-coast-through-geological-oceanography","status":"publish","type":"post","link":"https:\/\/mlml.sjsu.edu\/student-life\/2011\/11\/14\/learning-about-the-central-coast-through-geological-oceanography\/","title":{"rendered":"Learning About the Central Coast Through Geological Oceanography"},"content":{"rendered":"

By Catherine Drake<\/a>, Invertebrate Zoology Lab<\/p>\n

Other than a few awesome, albeit too short, trips to the Monterey Bay Aquarium, I hadn\u2019t spent much time in the Central Coast.\u00a0 So when I moved up here for graduate school at MLML, I didn\u2019t know much about the area; that is, until my MS 141 class.\u00a0 Geological Oceanography\u2014taught by Dr. Ivano Aiello\u2014involves learning about the formation of minerals and rocks, as well as geological mechanisms such as plate tectonics.\u00a0 We\u2019ve taken field trips almost every week to various locations along the Central Coast and inland as well.\u00a0 One of my favorite field trips was our overnight trip to Point Reyes, where we stayed in an old lifeboat station while we observed different types of rock formations.<\/p>\n

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The lifeboat station was built in 1927 at Chimeny Rock in Point Reyes.<\/figcaption><\/figure>\n

We examined multiple sedimentary rocks both along our journey to the station and also once we had arrived. \u00a0One of the depositions we inspected was an outcrop of radiolarian cherts.\u00a0 These deposits sit underneath about half of the Marin Headlands, are resistant to weathering, and can be up to 200 million years old.\u00a0 They are comprised of radiolarians, which are protozoans that form siliceous (made of silica) skeletons. \u00a0As these organisms decompose, a radiolarian ooze is formed in the deep ocean; over time, deposition occurs along the seafloor, forming the well-bedded radiolarian cherts.<\/p>\n

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Radiolarian cherts are formed from years of deposition of radiolarian siliceous skeletons on the seafloor.<\/figcaption><\/figure>\n

Igneous rocks were also on our list of stops, as we went to a formation of pillow basalts.\u00a0 They are formed underwater as lava comes in contact with seawater and cools rapidly. \u00a0Basalts are generally aphanitic rocks, meaning that they cool down too quickly for any minerals to form as the magma cools.\u00a0 As they are created, pillow basalts form ellipsoidal shapes and depict the direction of the lava flow.<\/p>\n

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Behind the class are pillow basalts, which are igneous rocks formed underwater as lava comes in contact with seawater and rapidly cools down.<\/figcaption><\/figure>\n

It was so surreal to touch igneous and sedimentary structures that formed hundreds of millions of years ago.\u00a0 Examining these rocks helped me better understand the geological mechanisms involved in their formation.\u00a0 Not only did these sedimentary depositions and igneous rocks help me become more acquainted with the Central Coast, but they also demonstrated the fact that oceans are integral components to the geologic history of our planet.<\/p>\n","protected":false},"excerpt":{"rendered":"

By Catherine Drake, Invertebrate Zoology Lab Other than a few awesome, albeit too short, trips to the Monterey Bay Aquarium, I hadn\u2019t spent much time in the Central Coast.\u00a0 So when I moved up here for graduate school at MLML, I didn\u2019t know much about the area; that is, until my MS 141 class.\u00a0 Geological […]<\/p>\n","protected":false},"author":291,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[130],"class_list":["post-5088","post","type-post","status-publish","format-standard","hentry","category-uncategorized","tag-geological-oceanography-lab"],"distributor_meta":false,"distributor_terms":false,"distributor_media":false,"distributor_original_site_name":"MLML Student Life","distributor_original_site_url":"https:\/\/mlml.sjsu.edu\/student-life","push-errors":false,"_links":{"self":[{"href":"https:\/\/mlml.sjsu.edu\/student-life\/wp-json\/wp\/v2\/posts\/5088","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/mlml.sjsu.edu\/student-life\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/mlml.sjsu.edu\/student-life\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/mlml.sjsu.edu\/student-life\/wp-json\/wp\/v2\/users\/291"}],"replies":[{"embeddable":true,"href":"https:\/\/mlml.sjsu.edu\/student-life\/wp-json\/wp\/v2\/comments?post=5088"}],"version-history":[{"count":0,"href":"https:\/\/mlml.sjsu.edu\/student-life\/wp-json\/wp\/v2\/posts\/5088\/revisions"}],"wp:attachment":[{"href":"https:\/\/mlml.sjsu.edu\/student-life\/wp-json\/wp\/v2\/media?parent=5088"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/mlml.sjsu.edu\/student-life\/wp-json\/wp\/v2\/categories?post=5088"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/mlml.sjsu.edu\/student-life\/wp-json\/wp\/v2\/tags?post=5088"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}