A visit to Central Coast of
California landed me to the complicated Franciscan Rocks that belong to the
Marin Headlands Terrane. The geology of the area is complex because of the
variety of stones present in the area. There is the sandstone which is a sedimentary
rock that is said to be a deposition from submarine landslides that happened at
the margins of the continent. The basalt rocks present are said to be the results
of the volcanoes that happened under the water. The other type of stone in the
area is the chert which is a combination of the shells rich in silica and
radiolarian that have single cells. The fourth and last type of stone in the
site is the serpentinite that is said to be formed when the earth`s upper
mantle alters.
Aside from the given geological map
of the area, I would also require aerial photographs, a compass and notes on
rock descriptions to complete the geological interpretation.
a)
Aerial photographs
Aerial
photographs which are pictures taken from the sky are very important in any
geological interpretation. Unlike common maps, the pictures give more detailed
information of an area making it easier to locate important features. The
photograph is also an exact representation of the site hence easier to read.
b)
Compass
With a
compass I will be able to survey the area in depth and measure the attitudes of
the geological features present in the site. A geological compass is called Brunton
and it is a combination of the compass, hand level, and the clinometers. Bearings
that are taken by a compass will help in giving a better interpretation of the
area because they will show the exact point to find a certain material.
c)
Rock description notes
The notes that contain all kinds of
rocks, where they are found and how they are characterized physically will
assist greatly in the geological interpretation of the site. The notes will
help confirm the word of the tour guide. It is also via the written notes that
we will be able to relate the class teachings to the existing geological structures.
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