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By Kristin Lynch
•This is an igneous rock.                 I was fairly sure this rock was granite,
•Granite is cooled intrusively (beneath   but decided to break it open with a
the surface of the Earth).                hammer and see the inside to be sure.
•The composition of granite is Sialic     Once broken, I could see the signature
with coarse grains and flecks of quartz   salt-and-pepper look of granite along
and potassium feldspar.                   with the shimmery flecks of quartz
                                          and potassium feldspar!
 I found this chunk of granite rock in a field in
  Hanford, California, near my workplace. There are
  many fields around the area and a variety of rocks can
  be found there. Yosemite National Park’s bedrock is
  formed mostly of granite. There are many formations
  (El Capitan, Cathedral Rocks, etc.) that are formed
  from this granite (Time). This chunk of granite is
  fairly large and I believe most likely came down from
  the Yosemite area.
I first identified this rock as a           Studying this rock in low light,
sedimentary rock, identified by its          one can see the few shimmery
several strata from compressed layers        flecks in the surface of the rock.
of sediment and brownish-gray color.
                                             The texture of the rock is not
                                             gritty, like the sedimentary rock
It is also very smooth in texture, most      sandstone, but instead is
likely from water. Further identified, I     extremely smooth. I assumed
believe this rock may be basalt.             this may be either from long
                                             exposure to wind or water. Some
                                             of the layers in the rock look like
                                             they are etched in and possibly
                                             disintegrating. This leads me to
                                             the conclusion that some layers
                                             of the sediment were not held
                                             together as strongly as the others
                                             due to the material they are
                                             made up of.
   This rock is extremely hard and would
    not break with a hammer. I had to use a
    sledge hammer to break it open. Once
    broken open, the layers that were so
    apparent on the outside of the rock
    became almost non-existent on the
    inside. The entire rock is extremely fine-
    grained and the inside is a dark grey and
    very shimmery. Because the shimmers
    are so many and so tiny, I would guess
    that they may be flecks of mica. There
    are flecks of mica in basalt. I also did the
    scratch test with this rock, and was not
    able to scratch it with a nail. Using a
    knife, I was able to scratch thin, shallow
    lines into the surface of the rock. Further    Outward appearance, this rock looks
    testing with vinegar, I dropped a couple       sedimentary, but the inside makes
    of drops onto the exterior surface, as well
    as the inside, and nothing happened.           me think metamorphic. Due to the
    This is common for basalt rocks, unless        physical properties and the tests that
    there are patches or bands of calcite,         I did on this rock, I concluded that
    which there weren’t in my rock.
                                                   this rock is the igneous rock, basalt.
 I found this intriguing and perplexing rock on a
 country road in Hanford, California while out taking
 photographs. If I correctly identified this rock as
 basalt, then it may be from the Lovejoy basalt, the
 largest eruptive unit in California. The Lovejoy flowed
 to the Sacramento Valley, which is very near to our
 Central Valley, where Hanford, California is located (A
 Mantle Plume).
This rock is white with semi-              I deduced that this rock
translucent high-shine flecks in it. In
this piece, there are a small amount of     was marble due to the
gray streaks and many medium-sized          color, shape, shining
crystals that glitter when light is         flecks, and scratch and
shined on it. I scratched this rock         vinegar tests. Marble is a
with a knife and white powder came          metamorphic rock that was
off easily. I also tried the white
vinegar test, which produced slight         once limestone. Limestone
bubbling.                                   is a sedimentary rock, but
                                            once exposed to high heat
                                            and pressure underground,
                                            it morphs into marble
                                            (Neighborhood Rocks:
                                            White Marble).
 I found this chunk of marble in another field between
 my house and work in Hanford, California. It really is
 a beautiful rock and it stood out in the field because of
 its stark white color and reflective flecks throughout
 the rock. I deduced that this rock probably came from
 someone’s garden/landscaping project because, after
 researching, I found that there aren’t any large marble
 areas around here. Marble chips are sold at home
 improvement stores and nurseries and are commonly
 found in landscaping.
 Kingdom: Animalia (animals)

  Phylum: Anthropoda (crustaceans,
   spiders, insects, and relatives)

     Class: Arachnida (arachnids)

      Order: Solpugida ( solpugids and sun
      spiders) (ADW)
 Sun spiders are otherwise known as
                                              camel spiders or wind scorpions.
                                              The names come from the color,
                                              humped back, or speed of the
                                              spider-like insect. These creatures
                                              are commonly found in the desert
                                              but they do not like the sun. It looks
                                              like a scorpion mixed with a spider,
                                              but it is not a spider. It uses its front
                                              legs (which are sticky) to grab its
                                              prey and pull it towards its pincers,
                                              which work like tiny saws to liquefy
                                              it before consuming it. They are not
                                              venomous and usually go near
                                              humans merely to stand in the
 This sun spider was found in Hanford,        shade of their shadow (Cranshaw).
   CA, in a home improvement store.
 Since these insects are desert dwellers,
   I’m guessing this guy hitched a ride
from one of the seamen that came back
    from Navy business in Fallon, CA.
 Kingdom: Plantae
   Subkingdom: Tracheobionta
     Division: Magnoliophyta
       Class: Magnoliopsida
         Subclass: Magnoliidae
         Order: Papaverales
           Family: Papaveraceae
            Genus: Eschscholzia
              Species: Eschscholzia Californica
              (Biogeography)
 The California Poppy is the
                                       state flower for California
                                       and grows wild throughout
                                       the state. They flourish on
                                       hillsides and in grassy,
                                       sandy, or rocky areas that
                                       are dry. They grow
                                       primarily in Southern
                                       California, but are also
This poppy is growing in Hanford,      common up the coast
CA, located in the Central Valley,     through Oregon and into
     which is a very dry area.         Washington, as well as in
                                       Nevada, New Mexico, and
                                       the northern part of Baja,
                                       Mexico (Biogeography).
 The Kings River that runs
  through Kings County, Fresno
  County, and Kings Canyon
  National Park in California
  begins in the Sierra Nevada.
  Some parts of the river are
  dammed and much of the river
  is utilized for its
  agricultural/irrigation
  purposes. It has also carved
  one of the deepest canyons in
  North America, beginning in
  the Sierra Nevada and
  dropping more than 13,000ft to
  the upper limit to the Pine Flat
  Reservoir! (Friends of the
  River)
 This is a picture of what the
  part of Kings River looks
  like that runs near
  Lemoore, Ca. It is
  commonly utilized during
  the warmer months for
  rafting, floating, boating,
  and fishing. This part of
  the river is far from the
  Middle and North Forks
  that are more commonly
  known for its rafting
  opportunities.
References
A mantle plume beneath California? The mid-Miocene Lovejoy flood basalt, northern California . (n.d.).    Geological Society of America Special
    Papers        . Retrieved November 15, 2011, from http://specialpapers.gsapubs.org/content/438/551.abstract
ADW: Eremobatidae: Classification. (n.d.). Animal Diversity Web. Retrieved November 18, 2011, from
   http://animaldiversity.ummz.umich.edu/site/accounts/classification/path/Eremobatidae.html#Eremobatidae
Biogeography of the California Poppy. (n.d.). redirect. Retrieved November 18, from
    http://bss.sfsu.edu/holzman/courses/Fall02%20projects/calpoppy.html
Cranshaw, W. (n.d.). Sunspiders (Windscorpions). Colorado State University Extension. Retrieved November 18, 2011, from
    http://www.ext.colostate.edu/pubs/insect/05589.html
Friends of the River: California Rivers - Kings River. (n.d.). Friends of the River: Home Preserve Restore Sustain California Rivers. Retrieved
     November 18, 2011, from http://www.friendsoftheriver.org/site/PageServer?pagename=FORCalRiversKingsRiver
Neighborhood Rocks: Gray Slate. (n.d.). Salt the Sandbox: Home Page. Retrieved November 18, 2011, from
    http://saltthesandbox.org/rocks/grayslate.htm
Neighborhood Rocks: Scoria Basalt. (n.d.). Salt the Sandbox: Home Page. Retrieved November 12, 2011, from
    http://saltthesandbox.org/rocks/basalt.htm
Neighborhood Rocks: White Marble. (n.d.). Salt the Sandbox: Home Page. Retrieved November 12, 2011, from
    http://saltthesandbox.org/rocks/whitemarble.htm#HowFormed
claystone (geology) -- Britannica Online Encyclopedia. (n.d.). Encyclopedia - Britannica Online Encyclopedia. Retrieved December 1, 2011, from
     http://www.britannica.com/EBchecked/topic/120751/claystone
time, m. C., & ago, a. f. (n.d.). CVO Menu - America's Volcanic Past - Yosemite. USGS Cascades Volcano Observatory (CVO). Retrieved December 1,
     2011, from http://vulcan.wr.usgs.gov/LivingWith/VolcanicPast/Places/volcanic_past_yosemite.html

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Geology rocks!

  • 2. •This is an igneous rock. I was fairly sure this rock was granite, •Granite is cooled intrusively (beneath but decided to break it open with a the surface of the Earth). hammer and see the inside to be sure. •The composition of granite is Sialic Once broken, I could see the signature with coarse grains and flecks of quartz salt-and-pepper look of granite along and potassium feldspar. with the shimmery flecks of quartz and potassium feldspar!
  • 3.  I found this chunk of granite rock in a field in Hanford, California, near my workplace. There are many fields around the area and a variety of rocks can be found there. Yosemite National Park’s bedrock is formed mostly of granite. There are many formations (El Capitan, Cathedral Rocks, etc.) that are formed from this granite (Time). This chunk of granite is fairly large and I believe most likely came down from the Yosemite area.
  • 4. I first identified this rock as a  Studying this rock in low light, sedimentary rock, identified by its one can see the few shimmery several strata from compressed layers flecks in the surface of the rock. of sediment and brownish-gray color. The texture of the rock is not gritty, like the sedimentary rock It is also very smooth in texture, most sandstone, but instead is likely from water. Further identified, I extremely smooth. I assumed believe this rock may be basalt. this may be either from long exposure to wind or water. Some of the layers in the rock look like they are etched in and possibly disintegrating. This leads me to the conclusion that some layers of the sediment were not held together as strongly as the others due to the material they are made up of.
  • 5. This rock is extremely hard and would not break with a hammer. I had to use a sledge hammer to break it open. Once broken open, the layers that were so apparent on the outside of the rock became almost non-existent on the inside. The entire rock is extremely fine- grained and the inside is a dark grey and very shimmery. Because the shimmers are so many and so tiny, I would guess that they may be flecks of mica. There are flecks of mica in basalt. I also did the scratch test with this rock, and was not able to scratch it with a nail. Using a knife, I was able to scratch thin, shallow lines into the surface of the rock. Further Outward appearance, this rock looks testing with vinegar, I dropped a couple sedimentary, but the inside makes of drops onto the exterior surface, as well as the inside, and nothing happened. me think metamorphic. Due to the This is common for basalt rocks, unless physical properties and the tests that there are patches or bands of calcite, I did on this rock, I concluded that which there weren’t in my rock. this rock is the igneous rock, basalt.
  • 6.  I found this intriguing and perplexing rock on a country road in Hanford, California while out taking photographs. If I correctly identified this rock as basalt, then it may be from the Lovejoy basalt, the largest eruptive unit in California. The Lovejoy flowed to the Sacramento Valley, which is very near to our Central Valley, where Hanford, California is located (A Mantle Plume).
  • 7. This rock is white with semi-  I deduced that this rock translucent high-shine flecks in it. In this piece, there are a small amount of was marble due to the gray streaks and many medium-sized color, shape, shining crystals that glitter when light is flecks, and scratch and shined on it. I scratched this rock vinegar tests. Marble is a with a knife and white powder came metamorphic rock that was off easily. I also tried the white vinegar test, which produced slight once limestone. Limestone bubbling. is a sedimentary rock, but once exposed to high heat and pressure underground, it morphs into marble (Neighborhood Rocks: White Marble).
  • 8.  I found this chunk of marble in another field between my house and work in Hanford, California. It really is a beautiful rock and it stood out in the field because of its stark white color and reflective flecks throughout the rock. I deduced that this rock probably came from someone’s garden/landscaping project because, after researching, I found that there aren’t any large marble areas around here. Marble chips are sold at home improvement stores and nurseries and are commonly found in landscaping.
  • 9.  Kingdom: Animalia (animals)  Phylum: Anthropoda (crustaceans, spiders, insects, and relatives)  Class: Arachnida (arachnids)  Order: Solpugida ( solpugids and sun spiders) (ADW)
  • 10.  Sun spiders are otherwise known as camel spiders or wind scorpions. The names come from the color, humped back, or speed of the spider-like insect. These creatures are commonly found in the desert but they do not like the sun. It looks like a scorpion mixed with a spider, but it is not a spider. It uses its front legs (which are sticky) to grab its prey and pull it towards its pincers, which work like tiny saws to liquefy it before consuming it. They are not venomous and usually go near humans merely to stand in the This sun spider was found in Hanford, shade of their shadow (Cranshaw). CA, in a home improvement store. Since these insects are desert dwellers, I’m guessing this guy hitched a ride from one of the seamen that came back from Navy business in Fallon, CA.
  • 11.  Kingdom: Plantae  Subkingdom: Tracheobionta  Division: Magnoliophyta  Class: Magnoliopsida  Subclass: Magnoliidae Order: Papaverales Family: Papaveraceae Genus: Eschscholzia Species: Eschscholzia Californica (Biogeography)
  • 12.  The California Poppy is the state flower for California and grows wild throughout the state. They flourish on hillsides and in grassy, sandy, or rocky areas that are dry. They grow primarily in Southern California, but are also This poppy is growing in Hanford, common up the coast CA, located in the Central Valley, through Oregon and into which is a very dry area. Washington, as well as in Nevada, New Mexico, and the northern part of Baja, Mexico (Biogeography).
  • 13.  The Kings River that runs through Kings County, Fresno County, and Kings Canyon National Park in California begins in the Sierra Nevada. Some parts of the river are dammed and much of the river is utilized for its agricultural/irrigation purposes. It has also carved one of the deepest canyons in North America, beginning in the Sierra Nevada and dropping more than 13,000ft to the upper limit to the Pine Flat Reservoir! (Friends of the River)
  • 14.  This is a picture of what the part of Kings River looks like that runs near Lemoore, Ca. It is commonly utilized during the warmer months for rafting, floating, boating, and fishing. This part of the river is far from the Middle and North Forks that are more commonly known for its rafting opportunities.
  • 15.
  • 16. References A mantle plume beneath California? The mid-Miocene Lovejoy flood basalt, northern California . (n.d.). Geological Society of America Special Papers . Retrieved November 15, 2011, from http://specialpapers.gsapubs.org/content/438/551.abstract ADW: Eremobatidae: Classification. (n.d.). Animal Diversity Web. Retrieved November 18, 2011, from http://animaldiversity.ummz.umich.edu/site/accounts/classification/path/Eremobatidae.html#Eremobatidae Biogeography of the California Poppy. (n.d.). redirect. Retrieved November 18, from http://bss.sfsu.edu/holzman/courses/Fall02%20projects/calpoppy.html Cranshaw, W. (n.d.). Sunspiders (Windscorpions). Colorado State University Extension. Retrieved November 18, 2011, from http://www.ext.colostate.edu/pubs/insect/05589.html Friends of the River: California Rivers - Kings River. (n.d.). Friends of the River: Home Preserve Restore Sustain California Rivers. Retrieved November 18, 2011, from http://www.friendsoftheriver.org/site/PageServer?pagename=FORCalRiversKingsRiver Neighborhood Rocks: Gray Slate. (n.d.). Salt the Sandbox: Home Page. Retrieved November 18, 2011, from http://saltthesandbox.org/rocks/grayslate.htm Neighborhood Rocks: Scoria Basalt. (n.d.). Salt the Sandbox: Home Page. Retrieved November 12, 2011, from http://saltthesandbox.org/rocks/basalt.htm Neighborhood Rocks: White Marble. (n.d.). Salt the Sandbox: Home Page. Retrieved November 12, 2011, from http://saltthesandbox.org/rocks/whitemarble.htm#HowFormed claystone (geology) -- Britannica Online Encyclopedia. (n.d.). Encyclopedia - Britannica Online Encyclopedia. Retrieved December 1, 2011, from http://www.britannica.com/EBchecked/topic/120751/claystone time, m. C., & ago, a. f. (n.d.). CVO Menu - America's Volcanic Past - Yosemite. USGS Cascades Volcano Observatory (CVO). Retrieved December 1, 2011, from http://vulcan.wr.usgs.gov/LivingWith/VolcanicPast/Places/volcanic_past_yosemite.html