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FIELD ASSIGNMENT
      PART 1
     By: Brittney Minor
COALINGA, CALIFORNIA
 Coalinga, California is located in the Great Valleys of California. Rock deposits are mostly
made up of sediments that have been brought here since the Jurassic, which is about 160 million
years ago, and continue to be deposited. There is a large quantity of oil fields located in the San
Joaquin Valley, and the little town of Coalinga is surrounded by them.
        •   http://www.conservation.ca.gov/cgs/information/publications/cgs_notes/note_36/Documents/note_36.pdf

 The Great Valley is composed mostly of Quaternary sedimentary deposits with a few
Tertiary and Quaternary volcanic rocks, and Mesozoic and Paleozoic metamorphic rocks;
including some Precambrian metamorphic rocks. On the west side of the Great Valley, where
Coalinga is located, there are also deposits of Tertiary sedimentary rocks, and Mesozoic
sedimentary rocks. Coalinga, California is located in one of the most diverse rock deposit beds in
the Great Valley.
        •   http://www.conservation.ca.gov/cgs/information/publications/cgs_notes/note_17/Documents/note_17.pdf
IGNEOUS ROCKS

 There are two different processes of which Igneous rocks form.
 Intrusive igneous rocks-rocks that are formed when lava cools and
crystalizes before it reaches the surface.
      • Examples include Granite, Diorite, and Gabbro.
 Extrusive igneous rocks-rocks that are formed when lava cools on the
surface, known as molten rock.
      • Examples include Rhyolite, Andesite, and Basalt.


       Earth an Introduction to Geology 10th Edition- Tarbuck, Lutgens, Tasa
IGNEOUS ROCKS
 I believe both samples to be Extrusive igneous rocks. After research
  I have concluded that the first sample is Andesite due to the texture
  and color. I have also come to the conclusion that the second
  sample is Basalt.




        Sample #1                                  Sample #2
METAMORPHIC ROCKS

 Metamorphic rocks change form. When the “parent rock” is exposed
to new conditions such as elevated temperatures and pressure that are
extremely different from what the rock is used to. These new elements
change the rock until it finds a new state of equilibrium. Heat can be a
factor, but if the rock completely melt, it would fall under the category of
igneous rock.


       Earth an Introduction to Geology 10th Edition- Tarbuck, Lutgens, Tasa
METAMORPHIC ROCK

 I believe sample #3 to be Slate because of the shape and texture. I
believe that Sample #4 is Quartzite due to texture and pattern.




Sample #3
                                                          Sample #4
SEDIMENTARY ROCK
 Sedimentary rocks are rocks that are formed from the weathered products of preexisting
rocks that are transported, deposited, and lithified.
    Detrital sedimentary rocks- rocks that are formed by whole particles being transported and
accumulated by chemical and mechanical weathering.
 Chemical sedimentary rocks- rocks that are formed of material that was precipitated from
water, whether it be by organic or inorganic means.
 Organic sedimentary rocks- rocks that are formed from organic material, such as plants.
They are normally found in the bottom of swamps. The primary example of organic
sedimentary rocks is coal.

         Earth an Introduction to Geology 10th Edition- Tarbuck, Lutgens, Tasa
SEDIMENTARY ROCKS

 I believe Sample #5 to be a piece of Travertine due to texture and
color patterns.

                          Sample #5
RESOURCES

 http://www.conservation.ca.gov/cgs/information/publications/c
gs_notes/note_36/Documents/note_36.pdf

 http://www.conservation.ca.gov/cgs/information/publications/c
   gs_notes/note_17/Documents/note_17.pdf

 Tarbuck, Lutgens, Tasa (2011) Earth an Introduction to Geology
10th Edition

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Field Assignment Part 1

  • 1. FIELD ASSIGNMENT PART 1 By: Brittney Minor
  • 2. COALINGA, CALIFORNIA  Coalinga, California is located in the Great Valleys of California. Rock deposits are mostly made up of sediments that have been brought here since the Jurassic, which is about 160 million years ago, and continue to be deposited. There is a large quantity of oil fields located in the San Joaquin Valley, and the little town of Coalinga is surrounded by them. • http://www.conservation.ca.gov/cgs/information/publications/cgs_notes/note_36/Documents/note_36.pdf  The Great Valley is composed mostly of Quaternary sedimentary deposits with a few Tertiary and Quaternary volcanic rocks, and Mesozoic and Paleozoic metamorphic rocks; including some Precambrian metamorphic rocks. On the west side of the Great Valley, where Coalinga is located, there are also deposits of Tertiary sedimentary rocks, and Mesozoic sedimentary rocks. Coalinga, California is located in one of the most diverse rock deposit beds in the Great Valley. • http://www.conservation.ca.gov/cgs/information/publications/cgs_notes/note_17/Documents/note_17.pdf
  • 3. IGNEOUS ROCKS  There are two different processes of which Igneous rocks form.  Intrusive igneous rocks-rocks that are formed when lava cools and crystalizes before it reaches the surface. • Examples include Granite, Diorite, and Gabbro.  Extrusive igneous rocks-rocks that are formed when lava cools on the surface, known as molten rock. • Examples include Rhyolite, Andesite, and Basalt.  Earth an Introduction to Geology 10th Edition- Tarbuck, Lutgens, Tasa
  • 4. IGNEOUS ROCKS  I believe both samples to be Extrusive igneous rocks. After research I have concluded that the first sample is Andesite due to the texture and color. I have also come to the conclusion that the second sample is Basalt. Sample #1 Sample #2
  • 5. METAMORPHIC ROCKS  Metamorphic rocks change form. When the “parent rock” is exposed to new conditions such as elevated temperatures and pressure that are extremely different from what the rock is used to. These new elements change the rock until it finds a new state of equilibrium. Heat can be a factor, but if the rock completely melt, it would fall under the category of igneous rock.  Earth an Introduction to Geology 10th Edition- Tarbuck, Lutgens, Tasa
  • 6. METAMORPHIC ROCK  I believe sample #3 to be Slate because of the shape and texture. I believe that Sample #4 is Quartzite due to texture and pattern. Sample #3 Sample #4
  • 7. SEDIMENTARY ROCK  Sedimentary rocks are rocks that are formed from the weathered products of preexisting rocks that are transported, deposited, and lithified.  Detrital sedimentary rocks- rocks that are formed by whole particles being transported and accumulated by chemical and mechanical weathering.  Chemical sedimentary rocks- rocks that are formed of material that was precipitated from water, whether it be by organic or inorganic means.  Organic sedimentary rocks- rocks that are formed from organic material, such as plants. They are normally found in the bottom of swamps. The primary example of organic sedimentary rocks is coal.  Earth an Introduction to Geology 10th Edition- Tarbuck, Lutgens, Tasa
  • 8. SEDIMENTARY ROCKS  I believe Sample #5 to be a piece of Travertine due to texture and color patterns. Sample #5
  • 9. RESOURCES  http://www.conservation.ca.gov/cgs/information/publications/c gs_notes/note_36/Documents/note_36.pdf  http://www.conservation.ca.gov/cgs/information/publications/c gs_notes/note_17/Documents/note_17.pdf  Tarbuck, Lutgens, Tasa (2011) Earth an Introduction to Geology 10th Edition