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Chancellor Tzomes
 GEL 103 7/29/12
INTRODUCTION
I am very fortunate to live in the city of FOLSOM, California.

It is located in Sacramento County and situated in the
westernmost foothills of the Sierra Nevada Mountains, on
the Southwest side of the American River in Northern
California.
There is a lot of rich history in the
geology and landscape of the area.
It sits 27 miles from Coloma, CA,
where gold was originally
discovered, and is about 85 miles
from Lake Tahoe, Nevada.

It’s most commonly known for its
gold rush history and prison.
FOLSOM HISTORY
Folsom has rich Western expansion history, with the California Gold
Rush and arrival of the railroad. Gold was first discovered along the
south bank of the American River in the area known as Negro Bar.
The discovery led to huge gold mining operations, along with the
need for a rail service (“Celebrating”, n.d.).

                                It’s named in honor after U.S. Army
                                           Captain, Joseph Folsom,
                               who purchased the land in 1847 and
                                 established the town for supporting
                                   gold mining and dredging activity.
                            The area is surrounded by rolling hills,
                                 and was the final destination of the
                Pony Express (from Missouri) when it was functional
                                                   in the mid-1800s.
FOLSOM STATE RECREATION AREA
The Folsom Lake State Recreation Area (FSRA) is a massive
reservoir that Was formed by the Folsom Dam, constructed in 1955 to
control the American River. It has over 11,500 surface acres, almost
75 miles of shoreline, and was placed just below the convergence of
the north and south forks of
The American River.

The dam and lake are both
part of the “Folsom Project”,
which provides flood control,
drinking water, irrigation,
And hydroelectricity to the
area (Crockett, n.d.).
FSRA GEOLOGY
The Folsom Lake State Recreation Area is located between
the central Sierra Nevada and the Central Valley geomorphic
provinces. The Sierra Nevada is characterized by a north-
northwest trending mountain belt with a broad region of
foothills along the western gradient. Located above the
Folsom Dam, it occupies the lower sections of canyons of
the North and South Forks of the American River, with a
peninsula stretching between the two arms of the lake.

Lake Natoma, located downstream from the dam occupies a
broad river valley that is cut into sedimentary rocks, and
ends at another dam called the Nimbus Dam. It occupies
the stretch between both dams.
FSRA GEOLOGY
Three major geologic divisions occur in the area:
   A north-northwest belt of metamorphic rocks with
    included ultramafic rocks (dense, rich in iron and
    magnesium).
   Granitic plutons that intruded and destroyed some of
    the metamorphic belt.
   Low-lying deposits of volcanic ash, debris flow, and
    alluvial fan deposits that overlie the older rocks.

      These divisions have created a varied and interesting
         geology for the area (“Environmental Conditions”, 2003).
FSRA GEOLOGY
There are four primary rock divisions found in
the area:
 Ultramafic
 Methamorphics
 Granodioriteand Granitic
 Volcanic Mud Flows

 Each is linked with a particular part of tectonic history, and
              each has distinct mineral resources
                   (“Environmental Conditions”, 2003).
FSRA GEOLOGY
   Ultramafic rocks - The ones found here represent the lowest part
    of the Earth’s crust, and have been lifted as much as 20 miles
    vertically by the faulting and regression of other pieces of crust –
    most likely when it was added to North America by accretion.
    Minerals associated with the rocks in the area include chromite,
    talc, asbestos, and nickel (“Environmental Conditions”, 2003).

   Metamorphics – are bands of metamorphosed sediments and
    igneous rocks that occur through most of the peninsula and
    southern area of the lake. They represent ancient chains of
    volcanic island arcs and the respective seafloor sediments over a
    long time period (Jurassic and Cretaceous). The terranes are
    separated by faults, and the age of these rocks go back over 160
    million years. Minerals associated with the rocks in the area
    include copper, zinc, and gold (“Environmental Conditions”, 2003).
FSRA GEOLOGY
   Granodiorite/Granitic rocks – slightly different than granite, they
    have slightly more iron and magnesium producing materials, and
    less quartz than granite. The crystals range in size, and the rock
    is coarse with a grainy appearance. The granitic rocks actually
    form the core of the Sierra Nevada, cooled from rock melted
    during the subduction process.
   Volcanic Mud Flows – the west side
    of Lake Natoma (area below the Dam)
    volcanically collected sediments mixed
    with volcanic mudflows
    (Miocene – Pliocene aged). Above them
    is a sequence of gravel, sand, and slit
    derived from granitic and metamorphic sources
    by way of debris flow and stream deposits –
    called the “Laguna Formation” (Pilocene aged) (Clark, 1970).
FSRA WILDLIFE




Rabbits, raccoons, skunks, possums, deer, grey foxes, geese, and
coyotes are regularly seen in the park and surrounding area. The
park also houses California horned lizards and western pond
turtles. Mountain lions, bobcats, and rattlesnakes also frequent
the area but are rarely seen (“Folsom Lake”, n.d.).
FSRA PLANTLIFE
           The area is abundant with
           oak trees (live & blue) and
                    foothill pine trees.
          Wildflowers bloom all during
               the spring and summer
                       (“Folsom Lake”, n.d.).
BIKE AND PEOPLE TRAILS
FSRA also maintains 34 miles of bike and pedestrian trails
which follow various creeks, dredger trails, and riverbank
forests. Many of the trails intersect the city’s open space
areas, greenbelts, and wetland areas.

The “American River Trail” is
considered to be one of the finest bike
trails in the state of California. It loops
under the Folsom Lake crossing and
continues alongside the west
shoreline of the American River.
There are incredible views of the river
and surrounding habitat such as the
oak trees, granite rocks, native
vegetation and wildlife (“Discover”, n.d.).
MY FIELD RESEARCH
During my exploration around FSRA, I located granodiorite, granitic, and
metamorphic rocks. I also located California Pine and Oak trees, and
spotted geese swimming along the riverbank.

  ALL of the following pictures were taken by me with my own camera!




         View from above Folsom Lake       View from Folsom Lake (ground level)
MY FIELD RESEARCH



  Trees behind me (including Oak)   Metamorphic rocks right in front of me.




            A better view.                      I HAD to touch it!
MY FIELD RESEARCH
MY FIELD RESEARCH



   This looks like Granite!      It IS Granite!




                              The ground nearby.
MY FIELD RESEARCH
          Video below (auto play)!
MY FIELD RESEARCH



  Looking east at the rolling foothills.   Alongside Folsom-Dam Road.




           This granite is HUGE!              Almost my size. Yikes!
MY FIELD RESEARCH



        Looks like Granodiorite.




  The Folsom Dam – close as I could get.   Base of the dam. Lots of granite beds.
MY FIELD RESEARCH



  Downstream from dam. Prison on left.    There’s granite everywhere in Folsom!




          California Pine Tree.          California Pine along the American River.
MY FIELD RESEARCH



    The American River.       Upstream (towards Folsom Dam).




   All along the riverbank.      Underneath an Oak Tree.
MY FIELD RESEARCH



Furthest downstream at Nimbus Dam. Facing upstream,   Geese came right up to me!
               eastern foothills in back.




                 All along the riverbank.                   Nimbus Dam.
SELECT LIST OF REFERENES
City of Folsom: Celebrating Folsom’s Rich History (n.d.). Retrieved from:
     www.folsom.ca.us/about/history.asp.

Discover Folsom.com: Recreation, Folsom Trails (n.d.). Retrieved from:
    www.discoverfolsom.com/recreation/folsom-trails/.

Geotechnical Consultants, Inc. (2003). Environmental Conditions Geology: Folsom Lake State Recreation
    Area. Retrieved from: www.parks.ca.gov/pages/files/Geology.pdf.

Golden Gate: Granitic and Grandiorite FAQ (n.d.). Retrieved from: www.nps.gov/goga/forteachers/granite-
    and-granodiorite-faq.htm.

Parks Guide: Folsom Lake State Recreation Area (n.d). Retrieved from: www.parksguide.com/folsom-
    lake-state-recreation-area/.

Todd Crockett (n.d.). Folsom Lake Information Guide: Folsom Lake-Good Fishing for Sacramento
    Residents. Retrieved from: http://www.jimporter.org/lakes/folsum/.

W.B. Clark, (1970). Gold Districts of California: California Department of Conservation, Division of Mines
    and Geology, Bulletin 193. Retrieved from: http://museumca.org/goldrush/dist-folsom.html.

Wikipedia: Folsom, California (n.d.). Retrieved from:
    www.en.wikipedia.org/wiki/Folsom,_California.

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Folsom Lake State Recreation Area

  • 1. Chancellor Tzomes GEL 103 7/29/12
  • 2. INTRODUCTION I am very fortunate to live in the city of FOLSOM, California. It is located in Sacramento County and situated in the westernmost foothills of the Sierra Nevada Mountains, on the Southwest side of the American River in Northern California. There is a lot of rich history in the geology and landscape of the area. It sits 27 miles from Coloma, CA, where gold was originally discovered, and is about 85 miles from Lake Tahoe, Nevada. It’s most commonly known for its gold rush history and prison.
  • 3. FOLSOM HISTORY Folsom has rich Western expansion history, with the California Gold Rush and arrival of the railroad. Gold was first discovered along the south bank of the American River in the area known as Negro Bar. The discovery led to huge gold mining operations, along with the need for a rail service (“Celebrating”, n.d.). It’s named in honor after U.S. Army Captain, Joseph Folsom, who purchased the land in 1847 and established the town for supporting gold mining and dredging activity. The area is surrounded by rolling hills, and was the final destination of the Pony Express (from Missouri) when it was functional in the mid-1800s.
  • 4. FOLSOM STATE RECREATION AREA The Folsom Lake State Recreation Area (FSRA) is a massive reservoir that Was formed by the Folsom Dam, constructed in 1955 to control the American River. It has over 11,500 surface acres, almost 75 miles of shoreline, and was placed just below the convergence of the north and south forks of The American River. The dam and lake are both part of the “Folsom Project”, which provides flood control, drinking water, irrigation, And hydroelectricity to the area (Crockett, n.d.).
  • 5. FSRA GEOLOGY The Folsom Lake State Recreation Area is located between the central Sierra Nevada and the Central Valley geomorphic provinces. The Sierra Nevada is characterized by a north- northwest trending mountain belt with a broad region of foothills along the western gradient. Located above the Folsom Dam, it occupies the lower sections of canyons of the North and South Forks of the American River, with a peninsula stretching between the two arms of the lake. Lake Natoma, located downstream from the dam occupies a broad river valley that is cut into sedimentary rocks, and ends at another dam called the Nimbus Dam. It occupies the stretch between both dams.
  • 6. FSRA GEOLOGY Three major geologic divisions occur in the area:  A north-northwest belt of metamorphic rocks with included ultramafic rocks (dense, rich in iron and magnesium).  Granitic plutons that intruded and destroyed some of the metamorphic belt.  Low-lying deposits of volcanic ash, debris flow, and alluvial fan deposits that overlie the older rocks. These divisions have created a varied and interesting geology for the area (“Environmental Conditions”, 2003).
  • 7. FSRA GEOLOGY There are four primary rock divisions found in the area:  Ultramafic  Methamorphics  Granodioriteand Granitic  Volcanic Mud Flows Each is linked with a particular part of tectonic history, and each has distinct mineral resources (“Environmental Conditions”, 2003).
  • 8. FSRA GEOLOGY  Ultramafic rocks - The ones found here represent the lowest part of the Earth’s crust, and have been lifted as much as 20 miles vertically by the faulting and regression of other pieces of crust – most likely when it was added to North America by accretion. Minerals associated with the rocks in the area include chromite, talc, asbestos, and nickel (“Environmental Conditions”, 2003).  Metamorphics – are bands of metamorphosed sediments and igneous rocks that occur through most of the peninsula and southern area of the lake. They represent ancient chains of volcanic island arcs and the respective seafloor sediments over a long time period (Jurassic and Cretaceous). The terranes are separated by faults, and the age of these rocks go back over 160 million years. Minerals associated with the rocks in the area include copper, zinc, and gold (“Environmental Conditions”, 2003).
  • 9. FSRA GEOLOGY  Granodiorite/Granitic rocks – slightly different than granite, they have slightly more iron and magnesium producing materials, and less quartz than granite. The crystals range in size, and the rock is coarse with a grainy appearance. The granitic rocks actually form the core of the Sierra Nevada, cooled from rock melted during the subduction process.  Volcanic Mud Flows – the west side of Lake Natoma (area below the Dam) volcanically collected sediments mixed with volcanic mudflows (Miocene – Pliocene aged). Above them is a sequence of gravel, sand, and slit derived from granitic and metamorphic sources by way of debris flow and stream deposits – called the “Laguna Formation” (Pilocene aged) (Clark, 1970).
  • 10. FSRA WILDLIFE Rabbits, raccoons, skunks, possums, deer, grey foxes, geese, and coyotes are regularly seen in the park and surrounding area. The park also houses California horned lizards and western pond turtles. Mountain lions, bobcats, and rattlesnakes also frequent the area but are rarely seen (“Folsom Lake”, n.d.).
  • 11. FSRA PLANTLIFE The area is abundant with oak trees (live & blue) and foothill pine trees. Wildflowers bloom all during the spring and summer (“Folsom Lake”, n.d.).
  • 12. BIKE AND PEOPLE TRAILS FSRA also maintains 34 miles of bike and pedestrian trails which follow various creeks, dredger trails, and riverbank forests. Many of the trails intersect the city’s open space areas, greenbelts, and wetland areas. The “American River Trail” is considered to be one of the finest bike trails in the state of California. It loops under the Folsom Lake crossing and continues alongside the west shoreline of the American River. There are incredible views of the river and surrounding habitat such as the oak trees, granite rocks, native vegetation and wildlife (“Discover”, n.d.).
  • 13. MY FIELD RESEARCH During my exploration around FSRA, I located granodiorite, granitic, and metamorphic rocks. I also located California Pine and Oak trees, and spotted geese swimming along the riverbank. ALL of the following pictures were taken by me with my own camera! View from above Folsom Lake View from Folsom Lake (ground level)
  • 14. MY FIELD RESEARCH Trees behind me (including Oak) Metamorphic rocks right in front of me. A better view. I HAD to touch it!
  • 16. MY FIELD RESEARCH This looks like Granite! It IS Granite! The ground nearby.
  • 17. MY FIELD RESEARCH Video below (auto play)!
  • 18. MY FIELD RESEARCH Looking east at the rolling foothills. Alongside Folsom-Dam Road. This granite is HUGE! Almost my size. Yikes!
  • 19. MY FIELD RESEARCH Looks like Granodiorite. The Folsom Dam – close as I could get. Base of the dam. Lots of granite beds.
  • 20. MY FIELD RESEARCH Downstream from dam. Prison on left. There’s granite everywhere in Folsom! California Pine Tree. California Pine along the American River.
  • 21. MY FIELD RESEARCH The American River. Upstream (towards Folsom Dam). All along the riverbank. Underneath an Oak Tree.
  • 22. MY FIELD RESEARCH Furthest downstream at Nimbus Dam. Facing upstream, Geese came right up to me! eastern foothills in back. All along the riverbank. Nimbus Dam.
  • 23. SELECT LIST OF REFERENES City of Folsom: Celebrating Folsom’s Rich History (n.d.). Retrieved from: www.folsom.ca.us/about/history.asp. Discover Folsom.com: Recreation, Folsom Trails (n.d.). Retrieved from: www.discoverfolsom.com/recreation/folsom-trails/. Geotechnical Consultants, Inc. (2003). Environmental Conditions Geology: Folsom Lake State Recreation Area. Retrieved from: www.parks.ca.gov/pages/files/Geology.pdf. Golden Gate: Granitic and Grandiorite FAQ (n.d.). Retrieved from: www.nps.gov/goga/forteachers/granite- and-granodiorite-faq.htm. Parks Guide: Folsom Lake State Recreation Area (n.d). Retrieved from: www.parksguide.com/folsom- lake-state-recreation-area/. Todd Crockett (n.d.). Folsom Lake Information Guide: Folsom Lake-Good Fishing for Sacramento Residents. Retrieved from: http://www.jimporter.org/lakes/folsum/. W.B. Clark, (1970). Gold Districts of California: California Department of Conservation, Division of Mines and Geology, Bulletin 193. Retrieved from: http://museumca.org/goldrush/dist-folsom.html. Wikipedia: Folsom, California (n.d.). Retrieved from: www.en.wikipedia.org/wiki/Folsom,_California.