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By. Luis Santillan
 The san Joaquin river traverses two geologic provinces in
  California that could not be more different which are the
  high mountains and exposed granitic rock of the southern
  Sierra Nevada and the topographically flat and sediment-
  filled Central Valley. The San Joaquin river is lined up
  along the 9,000-14,000 ft high spine of the Sierra cutting
  canyons and gorges from east to west across the
  mountains.
 The combinations of high elevations, eroding granite, and
  rivers is a lot of sediment. Its being over hundreds of
  thousands to millions of years, the erosion and transport of
  sediment from high country is balanced by deposition of
  that sediment in the adjacent low Central Valley. Over the
  geologic time the San Joaquin river has move around
  incrementally building up sediment and covering the
  entire valley as a result it is one of the worlds most
  productive agricultural regions.
 Igneous Rocks form when molten
 rock, called magma, cools and solidifies.
 as magma cools, crystal of various
 minerals form and grow. Coarse-grained
 igneous rocks that form far below the
 surface are called INTRUSIVE IGNEOUS
 ROCKS.




                                             (Tarbuck, 2008)
 I think that this rock is a granite a
  course-grained intrusive rock which is
  rick in the light-colored silicate minerals
  quartz and feldspar. Its an igneous rock
  that is especially abundant in Earth’s
  continental crust.



Sample # 1
 Minerals is any naturally occurring
 inorganic solid that possesses an orderly
 crystalline structure and a well-defined
 chemical composition. Minerals form by
 natural geologic processes. Inorganic
 crystalline solids, as exemplified by
 ordinary table salt are found naturally in
 the ground are considered minerals.




                                              (Tarbuck, 2008)
 Non-foliated metamorphic rock a Quartzite
 It does not have any layers and banded appearance
 I believe that this two rocks are Quartzites.
Example #2 and 3
 Sedimentary rocks are exposed at the
  surface more than igneous and
  metamorphic rocks. The most common
  sedimentary rocks are called detrital
  sedimentary rocks, the chemical
  sedimentary rocks and as the third
  category is organic sedimentary rocks.
 Sedimentary rocks have a wide variety of
  minerals and rock fragments that may
  be found in detrital rocks.




                                             (Tarbuck, 2008)
 As I found this rock at the lake shore I
  believe that this rock is a sandstone. The
  sand-size grains predominate as they
  form in a variety of environments and
  often contain significant clues of their
  origin such as sorting, particles shape
  and the composition.
Example #4
 Igneous rocks that form at the surface or
  as small masses within the upper crust
  where cooling is relatively rapid posses a
  very fine-grained texture termed
  APHANITIC. Crystals that make up
  aphanitic rocks are so small that
  individual minerals can only be
  distinguished with aid of a microscope.
 Some characteristics of the rocks is the
  fine grained rocks as being
  light, intermediate, or dark in color.


                                               (Tarbuck, 2008)
 This rock I believe is called Rhyolite, its
  an aphanitic type rock. Rhyolite is the
  extrusive equivalent of granite and like
  granite which is composed essentially of
  the light-colored silicates.

Example #5
 A fault is a fracture along which the blocks of crust on
   either side have moved relative to one another parallel
   to a fracture.
 Here is a picture of the
Wallace Creek in which
We could see the
San Andreas Fault.
I got this image from
Geology.com

            (Lynch, 2011)
 Mechanical weathering takes place when rocks are
  broken down without any change in the chemical
  nature of the rocks. Most of the rocks are torn apart
  basically by physical force instead of chemical
  breakdown.
 This photo was taken at
the Yosemite National
Park we could see the
Mechanical breakdown of
the rocks.
 The growing of bacteria such as of plants and tree
 roots will destroy a rock by digging their way down to
 its nooks and crannies, through this process the rock is
 forced apart causing it break into smaller pieces.




                                               (Godwin)
 I have two pictures of the
  Yosemite National Park
  and the other I had it on
  my phone since January
  when I went to my
  hometown in Mexico. At
  the moment I didn’t know
  I could of end up using it
  for this project. The water
  used from the cascade is
  distributed to the farms on
  the valley.
 The transitional
 sedimentary is found at
 the shoreline dividing the
 marine and the
 continental
 environments. Mass
 wasting or erosion causes
 the sediment that we can
 find at the shorelines.
 This picture is from my
 hometown in Mexico.
 I used the picture on the left because for what I
  understand the people say that it’s an eye of the pacific
  ocean I took it on January. The right hand-side picture
  was taken at the Monterey bay shore. I believe this two
  pictures are examples of the marine environment.
 This dam if I could call it
  like this, is very use full and
  practical to the residents in
  my hometown in Mexico
  they use it every day to give
  water to the cattle and is
  from the irrigation water
  comes from for farmers. Its
  as big as the dams we have
  here in the U.S but it surely
  provides enough water to
  the farmers.
 Lynch, D. (2011). Geology.com. Retrieved from
  http://geology.com/articles/san-andreas-fault.shtml
 Godwin, A. (n.d.). What are examples of mechanical
  weathering?. Retrieved from
  http://www.ehow.com/facts_6174539_examples-
  mechanical-weathering_.html

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Field lab assignment (luis santillan)

  • 2.  The san Joaquin river traverses two geologic provinces in California that could not be more different which are the high mountains and exposed granitic rock of the southern Sierra Nevada and the topographically flat and sediment- filled Central Valley. The San Joaquin river is lined up along the 9,000-14,000 ft high spine of the Sierra cutting canyons and gorges from east to west across the mountains.  The combinations of high elevations, eroding granite, and rivers is a lot of sediment. Its being over hundreds of thousands to millions of years, the erosion and transport of sediment from high country is balanced by deposition of that sediment in the adjacent low Central Valley. Over the geologic time the San Joaquin river has move around incrementally building up sediment and covering the entire valley as a result it is one of the worlds most productive agricultural regions.
  • 3.  Igneous Rocks form when molten rock, called magma, cools and solidifies. as magma cools, crystal of various minerals form and grow. Coarse-grained igneous rocks that form far below the surface are called INTRUSIVE IGNEOUS ROCKS. (Tarbuck, 2008)
  • 4.  I think that this rock is a granite a course-grained intrusive rock which is rick in the light-colored silicate minerals quartz and feldspar. Its an igneous rock that is especially abundant in Earth’s continental crust. Sample # 1
  • 5.  Minerals is any naturally occurring inorganic solid that possesses an orderly crystalline structure and a well-defined chemical composition. Minerals form by natural geologic processes. Inorganic crystalline solids, as exemplified by ordinary table salt are found naturally in the ground are considered minerals. (Tarbuck, 2008)
  • 6.  Non-foliated metamorphic rock a Quartzite  It does not have any layers and banded appearance  I believe that this two rocks are Quartzites. Example #2 and 3
  • 7.  Sedimentary rocks are exposed at the surface more than igneous and metamorphic rocks. The most common sedimentary rocks are called detrital sedimentary rocks, the chemical sedimentary rocks and as the third category is organic sedimentary rocks.  Sedimentary rocks have a wide variety of minerals and rock fragments that may be found in detrital rocks. (Tarbuck, 2008)
  • 8.  As I found this rock at the lake shore I believe that this rock is a sandstone. The sand-size grains predominate as they form in a variety of environments and often contain significant clues of their origin such as sorting, particles shape and the composition. Example #4
  • 9.  Igneous rocks that form at the surface or as small masses within the upper crust where cooling is relatively rapid posses a very fine-grained texture termed APHANITIC. Crystals that make up aphanitic rocks are so small that individual minerals can only be distinguished with aid of a microscope.  Some characteristics of the rocks is the fine grained rocks as being light, intermediate, or dark in color. (Tarbuck, 2008)
  • 10.  This rock I believe is called Rhyolite, its an aphanitic type rock. Rhyolite is the extrusive equivalent of granite and like granite which is composed essentially of the light-colored silicates. Example #5
  • 11.
  • 12.  A fault is a fracture along which the blocks of crust on either side have moved relative to one another parallel to a fracture.  Here is a picture of the Wallace Creek in which We could see the San Andreas Fault. I got this image from Geology.com (Lynch, 2011)
  • 13.  Mechanical weathering takes place when rocks are broken down without any change in the chemical nature of the rocks. Most of the rocks are torn apart basically by physical force instead of chemical breakdown.  This photo was taken at the Yosemite National Park we could see the Mechanical breakdown of the rocks.
  • 14.  The growing of bacteria such as of plants and tree roots will destroy a rock by digging their way down to its nooks and crannies, through this process the rock is forced apart causing it break into smaller pieces. (Godwin)
  • 15.
  • 16.
  • 17.  I have two pictures of the Yosemite National Park and the other I had it on my phone since January when I went to my hometown in Mexico. At the moment I didn’t know I could of end up using it for this project. The water used from the cascade is distributed to the farms on the valley.
  • 18.  The transitional sedimentary is found at the shoreline dividing the marine and the continental environments. Mass wasting or erosion causes the sediment that we can find at the shorelines. This picture is from my hometown in Mexico.
  • 19.  I used the picture on the left because for what I understand the people say that it’s an eye of the pacific ocean I took it on January. The right hand-side picture was taken at the Monterey bay shore. I believe this two pictures are examples of the marine environment.
  • 20.  This dam if I could call it like this, is very use full and practical to the residents in my hometown in Mexico they use it every day to give water to the cattle and is from the irrigation water comes from for farmers. Its as big as the dams we have here in the U.S but it surely provides enough water to the farmers.
  • 21.  Lynch, D. (2011). Geology.com. Retrieved from http://geology.com/articles/san-andreas-fault.shtml  Godwin, A. (n.d.). What are examples of mechanical weathering?. Retrieved from http://www.ehow.com/facts_6174539_examples- mechanical-weathering_.html