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Serpentinite at Madonna Inn

Hidden : 9/17/2008
Difficulty:
2.5 out of 5
Terrain:
1 out of 5

Size: Size: not chosen (not chosen)

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Geocache Description:

Serpentinite is relatively rare throughout most of the world but is somewhat common in Central and Northern California, so it was made the State Rock. This metamorphic rock is often bluish green and looks and feels waxy.

This outcrop is located behind the wine/gift shop of the Madonna Inn in San Luis Obispo. Permission has been granted to visit the site, but degradation, inappropriate activities, inconsiderate parking, etc. will get this location archived.

Often this rock is referred to as serpentine. However, it is actually called serpentinite and is made up of serpentine minerals. It is usually this distinctive bluish-green color, but can range from apple green to quite dark in other locations. A light and dark mottling is common. The shiny, waxy look is typical and has a slippery feel reminiscent of soap.

Up close, serpentinite looks either platy or fibrous depending upon which of the three most common serpentine minerals make up the rock. These minerals are lizardite, chrysotile, and antigorite. Lizardite and antigorite form platy (flat flakes) crystals while chrysotile forms fibrous (long strands) crystals. Fibrous chrysotile is the most common form of asbestos.

Serpentinite is a metamorphic rock. But unlike the majority of metamorphic rocks that form from increased heat and pressure, serpentinite forms most commonly when peridotite cools, encounters less pressure, and comes into contact with water. Peridotie is an igneous rock that is low in silica and high in magnesium and iron. Rocks having similar chemical composition are called mafic.

Mafic rocks typically form in the earth’s mantle below the crust. This deep in the earth, the temperature is very high and the pressure exerted by the overlying rock is very high. The minerals that form during these conditions are stable only under these conditions.

As the peridotie is pushed up into the crust at a mid-ocean spreading center and moves away, the temperature and pressure on the minerals is reduced. Fractures from plate movement and cooling rock create conduits for sea water to come into contact with the peridotie. Another major location where fractures are created is at subduction zones where the oceanic plate full of peridotie bends, forming additional cracks, and descends back into the mantle.

It is at subduction zones where serpentinite gets sheared off the subducting plate and attached to the continental plate. A subduction zone was present off the coast of California relatively recently. That is why serpentinite is common in California.

Now that the minerals that make up the peridotie are no longer in the high pressure and temperature conditions under which they are stable, they begin to metamorphose. Water is incorporated into the minerals and they become serpentine minerals turning the peridotie into serpentinite. The minerals brucite and magnetite are also formed with the magnesium and iron ions that are left over along with the release of hydrogen ions. Methane is formed as a by product of the formation of magnetite. This methamorphic process is called serpentization.

Serpentization increases the volume of the crystals by about 30%, thus decreasing the density of the rock. This further enlarges any cracks in the rock allowing more water to come into contact with unmetamorphosed peridotie, continuing the process deeper into the rock. This less dense rock begins to work its way up through more dense material above it, partially explaining how serpentintie is exposed at the earth’s surface.

Serpentization also creates heat in exothermic chemical reactions. The chemical reactions are capable increasing the temperature of the surrounding water by about 260 deg C (550 deg F). This creates deep undersea thermal vents as hot water is forced out of sea floor cracks pulling in cooler water. Entire undersea ecosystems have developed around these vents that are completely independent of the sun as the heat and food source (methane) is all derived from the chemical reactions of serpentization. It is thought that such ecosystems may have been important in the formation of early life.

Serpentization is also a major factor in the “deep” water cycle. That is discussed in a The Deep Water Cycle and Serpentininte.

Logging requirements:
Send me a note with :

  1. The text "GC1GBY3 Serpentinite at Madonna Inn" on the first line
  2. The number of people in your group.
  3. Closely examine the rock at the location and determine the type(s) of mineral(s) that likely make up the serpentinite
  4. Feel the rock surface and describe it texture and feel

The above information was compiled from the following sources:

  • California Geological Survey - CGS Note 41-Guidelines for Reviewing Geologic Reports; Serpentine: California State Rock; http://www.conservation.ca.gov/cgs/information/publications/cgs_notes/note_14/Pages/Index.aspx
  • Serpentine, Geohiking; http://www.geohiking.com/serpentine.html
  • Ask GeoMan...; http://jersey.uoregon.edu/~mstrick/AskGeoMan/geoQuerry45.html
  • The Deep Meaning of Lost City; A new type of vent sheds light on a major Earth process; By Andrew Alden, About.com ; http://geology.about.com/cs/escibasics/a/aa081003a.htm
  • Reaction Sea-water – Mantle: production of serpentine; http://www.ifremer.fr/serpentine/english/scientific-sheet-5.htm
  • SERPENTINE and SERPENTINITE, USGS, http://vulcan.wr.usgs.gov/LivingWith/VolcanicPast/Notes/serpentine.html

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Additional Hints (Decrypt)

V jbhyqa’g rkcbfr lbh gb n qnatrebhf zvareny

Decryption Key

A|B|C|D|E|F|G|H|I|J|K|L|M
-------------------------
N|O|P|Q|R|S|T|U|V|W|X|Y|Z

(letter above equals below, and vice versa)



 

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