Geology: It Really Rocks!

Geology is the study of the Earth’s structure and its substances. Some of our instructors focused on geology and marine geology in their college degrees. This week we want to focus on rocks! Because they rock (lol)!! On our planet there are three major types of rocks; metamorphic, igneous, and sedimentary.

serpentineGeologyMetamorphic rocks results from pressure, heat, stress, or a combination which changes an existing parent rock. Examples are schists; blue, green, and amphibolite. Consisting of many fine layers, these split easily and may be rich in mica. When a parent rock shale is heated to 300 °C, blue schist forms. When a parent rock shale is heated to 450 °C, green schist forms. When parent rock basalt is heated to 600 °C, amphibolite will form. The state rock of California is actually another type of metamorphic rock: serpentine!  Serpentine forms from a parent rock basalt when it is heated to 400 °C.

basaltIgneous rocks are the result of hot magma cooling and hardening. These can be intrusive or extrusive. Intrusive igneous occurs when magma cools underground, hardening slowly. This can produce large crystals. A local example is white microgranite, forming visible veins at Long Point, Catalina. Extrusive igneous rocks occur when magma cools quickly above ground due to air exposure, i.e. lava. Igneous RockThese crystals will be small, not necessarily visible. Here on Catalina we have red-brown basalt and red-white rhyolite, from the high peaks of the island, what once were volcanoes.

Sedimentary rocks are the result of rock particles or pieces of once living organism carried by water being deposited on land, river beds, lakes, beaches, and the ocean bottom. Eventually, these layers of particles are compacted into a new solid rock. Seventy-five percent of Earth’s surface rock are sedimentary. The fascinating types of sedimentary rocks composed of dead organic material such as plankton are called biogenous bottoms! Biogenous bottoms are sometimes referred to as oozes depending on the most common type of shell material in the sediments.

Geology

Calcareous OozesCalcareous oozes (calcium carbonate, calcite, limestone) result from a dominance of calcium shells which were originally from organisms such as foraminifera, snails, and sea urchins. These calcareous oozes are never found deeper than about 4,000 to 5,000 meters because the calcium dissolves at deeper depths.

Geology ShellsSiliceous oozes (silica, glass, diatoms, diatomaceous earth) results from a dominance of siliceous (glass) shell pieces made from planktonic organisms like diatoms and radiolarians. Where there are major plankton blooms with a sudden die off there are tremendous numbers of diatoms that reproduce and die each year contributing to the siliceous material on the sea floor. This shell material may build up at the rate of 1mm to 1cm every 1,000 years depending on the productivity.

Sources:

http://npic.orst.edu/factsheets/degen.html

https://www.nps.gov/subjects/geology/sedimentary.htm

Pictures:

https://commons.wikimedia.org/wiki/File:Diatom2.jpg

https://commons.wikimedia.org/wiki/File:Layers_of_sedimentary_rock_in_Makhtesh_Ramon_(50751).jpg

https://www.flickr.com/photos/jsjgeology/16940796272

https://commons.wikimedia.org/wiki/File:Basalt,_Lanzarote_J1.jpg

 

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We would like to thank you for visiting our blog. Catalina Island Marine Institute is a hands-on marine science program with an emphasis on ocean exploration. Our classes and activities are designed to inspire students toward future success in their academic and personal pursuits. This blog is intended to provide you with up-to-date news and information about our camp programs, as well as current science and ocean happenings. This blog has been created by our staff who have at least a Bachelors Degree usually in marine science or related subjects. We encourage you to also follow us on Facebook, Instagram, Google+, Twitter, and Vine to see even more of our interesting science and ocean information. Feel free to leave comments, questions, or share our blog with others. Please visit www.cimi.org for additional information. Happy Reading!

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