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GEOGRAPHY 5
PROJECT




           FIELD TRIPS 1 AND 2
DATE                               CLIENT
          OCT 6, NOV 16-18, 2012            JEANNETTE HERNANDEZ
Mormon Rocks
MORMON ROCKS WAS FORMED BY
WIND AND WATER EROSIONS. IT IS
LOCATED ON THE SAN ANDREAS
RIFT ZONE.




MORMON ROCKS ARE COMPOSED
OF SANDSTONE , BUT OVER THE
YEARS, A MIXTURE OF OTHER
ROCKS WERE BLENDED INTO THE
FOUNDATION.
Mormon Rocks
continued...
  EAST


            WEST


         THE SAN ANDREAS RIFT ZONE
         AND STREAM BED IS LOCATED
         NEAR THE CAJON PASS. THE FAULT
         IS STRIKE-SLIP ZONE WHERE THE
         NORTH AMERICAN PLATE AND THE
         PACIFIC PLATE COME TOGETHER.
Cinder Hill Volcano

This volcano is a
composite and is
inactive.
                       LAVA FLOW
The Lava flow is made
of Basaltic Lava.
Fossil Falls stream bed


             The image shows the
             dried stream bed of
             Owens Lake that went
             through fossil falls.
Fossil Falls

Fossil Falls was formed
by the volcanic activity
in the mountain range
and meltwater from
glaciers near the sierra
nevada.
Fossil Falls- Metate Holes
   and Obsidian Flakes




METATE HOLES WERE CREATED    THE OBSIDIAN FLAKES FOUND
BY WATER WHEN DEBRIS HIT     IN FOSSIL FALLS WERE LEFT
THE SAME AREA AND WOULD      BY THE NATIVES AS SCRAPS
CIRCULATE AGAINST THE ROCK   FROM THE TOOLS THEY WOULD
TO CREATE SMOOTH CIRCULAR    MAKE FROM THEM, SUCH AS,
HOLES.                       ARROW HEADS.
Fossil Falls- Petroglyph
and House Rings
A Petroglyph is a rock
carving. The one
pictured was created
by native americans.

The house ring was
used as living space
for the native
americans.
Mt. Whitney

              Mt. Whitney is located
              in the Sierra Nevada
              Mountain range and
              has the highest
              elevation of 14,505
              feet.
Inyo-White Mountains
Alluvial Fan
Diaz Lake

            DIAZ LAKE WAS
            FORMED BY THE
            1872 LONE PINE
            EARTHQUAKE THAT
            WAS THOUGHT TO BE
            A LEVEL 9.
Lone Pine Fault

18 MILES OF
OWEN’S VALLEY
DROPPED 20 FEET
BECAUSE OF THE
THE LONE PINE
EARTHQUAKE OF
1872
Manzanar

Manzanar is most widely known as the site of
one of ten camps where over 110,000
Japanese Americans were incarcerated during
World War II. Located at the foot of the Sierra
Nevada in California's Owens Valley between
the towns of Lone Pine to the south and
Independence to the north, it is approximately
230 miles (370 km) northeast of Los Angeles.
Manzanar (which means "apple orchard" in
Spanish) was identified by the United States
National Park Service as the best-preserved of
the former camp sites, and was designated the
Manzanar National Historic Site.
Mono Lake
                   NEGIT ISLAND




  PAOHA VOLCANIC
      ISLAND
Former Shorelines of
    Mono Lake

           THE DIFFERENT VEGETATION REPRESENTS
      THE FORMER SHORELINES. THE DIFFERENCE IN COLOR
            SHOWS WHAT USE TO BE UNDER WATER.
Former Shorelines of
Mono Lake Continued...
                       GOAL FOR NEW
                        SHORELINE




TUFA TOWERS FORMALLY
     UNDER WATER
Mono Lake Tufa Towers



Tufa is formed by
the precipitation of
carbonate minerals
from ambient
temperature water
bodies.
Panum Crater
Convict Lake



THE LAKE CREATION: DURING THE ICE AGE
GLACIERS FORMED THE SIERRA NEVADAS’.     OLDEST ROCK FORMATION
THE SIERRA NEVADAS’ PICKED UP ROCKS AS
RIVERS OF ICE MOVED DOWNHILL, MOUNDS
OF RUBLE (MORAINES) WERE DEPOSITED AT
THE ENDS AND ALONG THE SIDES OF
GLACIERS. A RETREATING GLACIER FROM
THE LAST ICE AGE LEFT BEHIND THE
MORAINE THAT DAMMED CONVICT CREEK,
HELPING FORM CONVICT LAKE.
Keoughs Hot Springs
       The hot
       springs were
       created from
       earthquake
       activity. As
       water flows
       through cracks
       created by
       earthquakes, it
       is heated by
       underground
       volcanic
       activity and
       pushed up.
June Lake Loop
                           WATERFALL




SILVER LAKE


              GRANT LAKE
Owens River
Eastern California
          Museum
I was very interested in
the old houses that the
people of Manzanar
use to live in. I have
always been a fan of
ghost towns and to
me, this felt like one.
Extra Credit
 In Transit
SOLAR POWER PLANT
SEGS III–VII at Kramer Junction
DOPPLER RADAR TOWER
A Doppler radar is a specialized radar that makes use of the Doppler effect to produce velocity data about objects at a distance. It
does this by beaming a microwave signal towards a desired target and listening for its reflection, then analyzing how the frequency of
the returned signal has been altered by the object's motion. This variation gives direct and highly accurate measurements of the radial
component of a target's velocity relative to the radar.
GARLOCK FAULT
The Garlock Fault is a left-lateral strike-slip fault running approximately northeast-southwest along the north margins of the Mojave
Desert of Southern California. It runs for much of its length along the southern base of the Tehachapi Mountains.
CREOSOTE




                                        BURROWEED GRASS




DESERT VEGETATION
JOSHUA TREE, CRESOTE, BURROWEED GRASS
CALIFORNIA AQUEDUCT
OWENS DRY LAKE
Owens held significant water until 1924, until much of the Owens River was diverted into the Los Angeles Aqueduct, causing it to
desiccate. Today, some of the flow of the river has been restored, and the lake now contains some water.

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Geography 5 photo journal

  • 1. GEOGRAPHY 5 PROJECT FIELD TRIPS 1 AND 2 DATE CLIENT OCT 6, NOV 16-18, 2012 JEANNETTE HERNANDEZ
  • 2. Mormon Rocks MORMON ROCKS WAS FORMED BY WIND AND WATER EROSIONS. IT IS LOCATED ON THE SAN ANDREAS RIFT ZONE. MORMON ROCKS ARE COMPOSED OF SANDSTONE , BUT OVER THE YEARS, A MIXTURE OF OTHER ROCKS WERE BLENDED INTO THE FOUNDATION.
  • 3. Mormon Rocks continued... EAST WEST THE SAN ANDREAS RIFT ZONE AND STREAM BED IS LOCATED NEAR THE CAJON PASS. THE FAULT IS STRIKE-SLIP ZONE WHERE THE NORTH AMERICAN PLATE AND THE PACIFIC PLATE COME TOGETHER.
  • 4. Cinder Hill Volcano This volcano is a composite and is inactive. LAVA FLOW The Lava flow is made of Basaltic Lava.
  • 5. Fossil Falls stream bed The image shows the dried stream bed of Owens Lake that went through fossil falls.
  • 6. Fossil Falls Fossil Falls was formed by the volcanic activity in the mountain range and meltwater from glaciers near the sierra nevada.
  • 7. Fossil Falls- Metate Holes and Obsidian Flakes METATE HOLES WERE CREATED THE OBSIDIAN FLAKES FOUND BY WATER WHEN DEBRIS HIT IN FOSSIL FALLS WERE LEFT THE SAME AREA AND WOULD BY THE NATIVES AS SCRAPS CIRCULATE AGAINST THE ROCK FROM THE TOOLS THEY WOULD TO CREATE SMOOTH CIRCULAR MAKE FROM THEM, SUCH AS, HOLES. ARROW HEADS.
  • 8. Fossil Falls- Petroglyph and House Rings A Petroglyph is a rock carving. The one pictured was created by native americans. The house ring was used as living space for the native americans.
  • 9. Mt. Whitney Mt. Whitney is located in the Sierra Nevada Mountain range and has the highest elevation of 14,505 feet.
  • 12. Diaz Lake DIAZ LAKE WAS FORMED BY THE 1872 LONE PINE EARTHQUAKE THAT WAS THOUGHT TO BE A LEVEL 9.
  • 13. Lone Pine Fault 18 MILES OF OWEN’S VALLEY DROPPED 20 FEET BECAUSE OF THE THE LONE PINE EARTHQUAKE OF 1872
  • 14. Manzanar Manzanar is most widely known as the site of one of ten camps where over 110,000 Japanese Americans were incarcerated during World War II. Located at the foot of the Sierra Nevada in California's Owens Valley between the towns of Lone Pine to the south and Independence to the north, it is approximately 230 miles (370 km) northeast of Los Angeles. Manzanar (which means "apple orchard" in Spanish) was identified by the United States National Park Service as the best-preserved of the former camp sites, and was designated the Manzanar National Historic Site.
  • 15. Mono Lake NEGIT ISLAND PAOHA VOLCANIC ISLAND
  • 16. Former Shorelines of Mono Lake THE DIFFERENT VEGETATION REPRESENTS THE FORMER SHORELINES. THE DIFFERENCE IN COLOR SHOWS WHAT USE TO BE UNDER WATER.
  • 17. Former Shorelines of Mono Lake Continued... GOAL FOR NEW SHORELINE TUFA TOWERS FORMALLY UNDER WATER
  • 18. Mono Lake Tufa Towers Tufa is formed by the precipitation of carbonate minerals from ambient temperature water bodies.
  • 20. Convict Lake THE LAKE CREATION: DURING THE ICE AGE GLACIERS FORMED THE SIERRA NEVADAS’. OLDEST ROCK FORMATION THE SIERRA NEVADAS’ PICKED UP ROCKS AS RIVERS OF ICE MOVED DOWNHILL, MOUNDS OF RUBLE (MORAINES) WERE DEPOSITED AT THE ENDS AND ALONG THE SIDES OF GLACIERS. A RETREATING GLACIER FROM THE LAST ICE AGE LEFT BEHIND THE MORAINE THAT DAMMED CONVICT CREEK, HELPING FORM CONVICT LAKE.
  • 21. Keoughs Hot Springs The hot springs were created from earthquake activity. As water flows through cracks created by earthquakes, it is heated by underground volcanic activity and pushed up.
  • 22. June Lake Loop WATERFALL SILVER LAKE GRANT LAKE
  • 24. Eastern California Museum I was very interested in the old houses that the people of Manzanar use to live in. I have always been a fan of ghost towns and to me, this felt like one.
  • 25. Extra Credit In Transit
  • 26. SOLAR POWER PLANT SEGS III–VII at Kramer Junction
  • 27. DOPPLER RADAR TOWER A Doppler radar is a specialized radar that makes use of the Doppler effect to produce velocity data about objects at a distance. It does this by beaming a microwave signal towards a desired target and listening for its reflection, then analyzing how the frequency of the returned signal has been altered by the object's motion. This variation gives direct and highly accurate measurements of the radial component of a target's velocity relative to the radar.
  • 28. GARLOCK FAULT The Garlock Fault is a left-lateral strike-slip fault running approximately northeast-southwest along the north margins of the Mojave Desert of Southern California. It runs for much of its length along the southern base of the Tehachapi Mountains.
  • 29. CREOSOTE BURROWEED GRASS DESERT VEGETATION JOSHUA TREE, CRESOTE, BURROWEED GRASS
  • 31. OWENS DRY LAKE Owens held significant water until 1924, until much of the Owens River was diverted into the Los Angeles Aqueduct, causing it to desiccate. Today, some of the flow of the river has been restored, and the lake now contains some water.

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  31. \n