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Rocio Villarreal Geography 5 Photo Journal
Cinder Hill, Fossil Falls, and Mormon Rocks April 2,2011 Field Trip #2
April 2, 2011 Cinder Hill
Also known as Red Hill, it is one of 21 active volcanoes in the Coso Volcanic Range.  Its last eruption was about 500 years ago.  April 2, 2011 Cinder Hill
Lava flows are extrusive volcanic formations made up of basalt. Basalt is the dark colored lava, and its color was caused by the rapid cooling of the lava when it reached the earth’s surface.  April 2, 2011 Lava Flows
Yellow Wildflower at Cinder Hill.
April 2, 2011 Fossil Falls
Owens Stream bed near Fossil Falls.  Water from Owens Lake used to run through here.  April 2, 2011 Owens Stream Bed
Fossil Falls was sculpted by lava and water about 44o,000 years ago from the result of a violent eruption.  April 2, 2011 Fossil Falls
Metate Holes were made by rocks that got stuck in lava, whirled around and carved a hole. April 2, 2011 Metate Holes
Obsidian  is a black, glass-like, type of rock that Native Americans used to make arrowheads.  April 2, 2011 Obsidian Flakes
Petroglyphs are writings on rocks that were drawn by Native Americans that lived around this area for about 10,000 years. This petroglyph contains a picture of big horn sheep and a Shaman. April 2, 2011 Petroglyphs
House rings were foundations for Native American homes.  April 2, 2011 House Ring
April 2, 2011 Rattlesnake Weed
April 2, 2011 Bluepine Bush
April 2, 2011 Mormon Rocks
Mormon Rocks is a tilted fault block, made by the San Andreas Fault, which brings together the Pacific Plate with the North American Plate.   April 2, 2011 Mormon Rocks
The Granular structure of Mormon Rocks is made up of sedimentary rock, and its layers show a perfect weather record of how much rain falls every year.  April 2, 2011  Granular Structure
San Andreas fault brings together the Pacific Plate with the North American Plate.  April 2, 2011 San Andreas Rift Zone and Stream Bed San Andreas Rift Zone Stream bed
The Yaka tree is related to Joshua trees.  April 2, 2011 Yaka Tree
Diaz Lake, Mt. Whitney Interagency Visitors Center, Keoughs	 Hot Springs, Mono Lake, Convict Lake, Owens River, Eastern California Museum, and Manzanar April 15-17, 2011 Field Trip #2
April 15, 2011 Diaz Lake
Diaz lake was made by an 8.0+ earthquake in 1872. During the earthquake, the earth sank and the land started to fill up with water. It is also known as a sag pond.  April 15, 2011 Diaz Lake Diaz Lake
The Lone Pine Fault is located next to Diaz lake.  April 15, 2011 Lone Pine Fault Sierra Nevada Aqueduct Lone Pine Fault
Near Diaz Lake.  April 15, 2011 Cottonwood Tree
April 15, 2011 Mt. Whitney Interagency Visitors Center
Mt. Whitney is located in the Sierra Nevada Mountains. Its elevation is 14,505 ft.  These mountains were formed by glaciers.  April 15, 2011 Mt. Whitney Mt. Whitney
Inyo Mountains used to be underwater and were pushed up out of the ocean because of the plate tectonics. They were sedimentary rock but as time passed they began to dry up and it turned into metamorphic rock.  April 15, 2011 Inyo-White Mountains Inyo-White Mountains
Alluvial Fan located in the Inyo-White Mountains.  April 15, 2011 Alluvial Fan Alluvial Fan Photo taken by: Jessica Esparza
April 15, 2011 Keoughs Hot Springs
This stream is a hot spring, water is heated from the fault that lies underneath. When the water is heated, it rises up and runs through a creek.  April 15, 2011 Stream
April 16, 2011 Mono Lake
Mono Lake has 2 islands, Negit and Paoha Island. Negit Island was a volcano and it last erupted about 800 years ago. Paoha Island rose from underneath the lake due to volcanic magma pushing up sediments above the surface of the lake.  April 16, 2011 Mono Lake Paoha Island Negit Island Mono Lake
Mono Lake has been drying over the years, and it started to dry up even faster when Los Angeles Dept. of Water and Power started to take the water from the streams that led up to Mono Lake.  Today a few of those streams had been restored and allow some water to go back in to Mono Lake.  April 16, 2011 Mono Lake Shorelines Ancient Shoreline Old Shoreline Recent Shoreline
April 16, 2011 Swallow
Tufas used to be underwater, they are made up of calcium, carbonate and lime, which were formed when fresh water and salt water meet.  It also shows where streams used to meet the lake.  April 16, 2011 Tufa
North America’s newest mountain range. It was made up by volcanoes, in which there are 110 in the area.  April 16,2011 Mono Crater
April 16, 2011 Convict Lake
Convict Lake got its name when convicts were found after they had escaped from prison and later  were hung by authorities in 1871. April 16, 2011 Convict Lake Oldest Rock Formation Lateral Moraine Convict Lake
A terminal is the sediment that was moved from it place by glaciers.  April 16, 2011 Terminal Terminal
April 16, 2011 Owens River
This benchmark is found next to the Owens River, near Bishop, California. April 16, 2011  Benchmark
Swallow nests are found underneath this bridge above the Owens River.  April 16, 2011 Owens River with Swallows nests Swallows Nests Owens River
Bristlecone trees are about 4500 years old and are the oldest living trees in the world.  April 16, 2011 Inyo-White Mountains with Bristlecones Bristlecones Inyo-White Mountains
April 17, 2011 Eastern California Museum
I chose this picture because it is part of a model of what a Japanese Internment camp would look like. Now not very many are still standing.  April 17, 2011 Internment Camp
April 17, 2011 Manzanar
Manzanar was one of ten labor camps in which people of Japanese decent were sent during World War II. About 110,000 men, women, and children lived here.  April 17, 2011 Manzanar  War Relocation Center
This is part of what is left of Manzanar. Most of its buildings and artifacts were removed from this camp and were used to build other buildings in the neighboring town, or sent to museums.  	April 17, 2011 Manzanar  Area
In-Transit Photos
Solar Power Plant April 2, 2011
Koehn Lake Desert Playa April 2, 2011
Doppler Radar Towers are used to measure wind.  Doppler Radar Tower April 2, 2011
Near Red Mountain, Rand Mining District. Mine Tailings
April 2, 2011 Garlock Fault
April 2, 2011 California Aqueduct
Mojave Desert Wildflowers April 2, 2011
April 15, 2011 Cucamonga Alluvial Fan Cucamonga Alluvial Fan
Desert Vegetation Joshua Tree Creosote  April 15, 2011
April 15, 2011 Desert Vegetation Burroweed Grass
April 15, 2011 Owens Dry Lake Owens Dry Lake
April 15, 2011 SETI Towers

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PhotoJournal Geo5 Lab

  • 1. Rocio Villarreal Geography 5 Photo Journal
  • 2. Cinder Hill, Fossil Falls, and Mormon Rocks April 2,2011 Field Trip #2
  • 3. April 2, 2011 Cinder Hill
  • 4. Also known as Red Hill, it is one of 21 active volcanoes in the Coso Volcanic Range. Its last eruption was about 500 years ago. April 2, 2011 Cinder Hill
  • 5. Lava flows are extrusive volcanic formations made up of basalt. Basalt is the dark colored lava, and its color was caused by the rapid cooling of the lava when it reached the earth’s surface. April 2, 2011 Lava Flows
  • 6. Yellow Wildflower at Cinder Hill.
  • 7. April 2, 2011 Fossil Falls
  • 8. Owens Stream bed near Fossil Falls. Water from Owens Lake used to run through here. April 2, 2011 Owens Stream Bed
  • 9. Fossil Falls was sculpted by lava and water about 44o,000 years ago from the result of a violent eruption. April 2, 2011 Fossil Falls
  • 10. Metate Holes were made by rocks that got stuck in lava, whirled around and carved a hole. April 2, 2011 Metate Holes
  • 11. Obsidian is a black, glass-like, type of rock that Native Americans used to make arrowheads. April 2, 2011 Obsidian Flakes
  • 12. Petroglyphs are writings on rocks that were drawn by Native Americans that lived around this area for about 10,000 years. This petroglyph contains a picture of big horn sheep and a Shaman. April 2, 2011 Petroglyphs
  • 13. House rings were foundations for Native American homes. April 2, 2011 House Ring
  • 14. April 2, 2011 Rattlesnake Weed
  • 15. April 2, 2011 Bluepine Bush
  • 16. April 2, 2011 Mormon Rocks
  • 17. Mormon Rocks is a tilted fault block, made by the San Andreas Fault, which brings together the Pacific Plate with the North American Plate. April 2, 2011 Mormon Rocks
  • 18. The Granular structure of Mormon Rocks is made up of sedimentary rock, and its layers show a perfect weather record of how much rain falls every year. April 2, 2011 Granular Structure
  • 19. San Andreas fault brings together the Pacific Plate with the North American Plate. April 2, 2011 San Andreas Rift Zone and Stream Bed San Andreas Rift Zone Stream bed
  • 20. The Yaka tree is related to Joshua trees. April 2, 2011 Yaka Tree
  • 21. Diaz Lake, Mt. Whitney Interagency Visitors Center, Keoughs Hot Springs, Mono Lake, Convict Lake, Owens River, Eastern California Museum, and Manzanar April 15-17, 2011 Field Trip #2
  • 22. April 15, 2011 Diaz Lake
  • 23. Diaz lake was made by an 8.0+ earthquake in 1872. During the earthquake, the earth sank and the land started to fill up with water. It is also known as a sag pond. April 15, 2011 Diaz Lake Diaz Lake
  • 24. The Lone Pine Fault is located next to Diaz lake. April 15, 2011 Lone Pine Fault Sierra Nevada Aqueduct Lone Pine Fault
  • 25. Near Diaz Lake. April 15, 2011 Cottonwood Tree
  • 26. April 15, 2011 Mt. Whitney Interagency Visitors Center
  • 27. Mt. Whitney is located in the Sierra Nevada Mountains. Its elevation is 14,505 ft. These mountains were formed by glaciers. April 15, 2011 Mt. Whitney Mt. Whitney
  • 28. Inyo Mountains used to be underwater and were pushed up out of the ocean because of the plate tectonics. They were sedimentary rock but as time passed they began to dry up and it turned into metamorphic rock. April 15, 2011 Inyo-White Mountains Inyo-White Mountains
  • 29. Alluvial Fan located in the Inyo-White Mountains. April 15, 2011 Alluvial Fan Alluvial Fan Photo taken by: Jessica Esparza
  • 30. April 15, 2011 Keoughs Hot Springs
  • 31. This stream is a hot spring, water is heated from the fault that lies underneath. When the water is heated, it rises up and runs through a creek. April 15, 2011 Stream
  • 32. April 16, 2011 Mono Lake
  • 33. Mono Lake has 2 islands, Negit and Paoha Island. Negit Island was a volcano and it last erupted about 800 years ago. Paoha Island rose from underneath the lake due to volcanic magma pushing up sediments above the surface of the lake. April 16, 2011 Mono Lake Paoha Island Negit Island Mono Lake
  • 34. Mono Lake has been drying over the years, and it started to dry up even faster when Los Angeles Dept. of Water and Power started to take the water from the streams that led up to Mono Lake. Today a few of those streams had been restored and allow some water to go back in to Mono Lake. April 16, 2011 Mono Lake Shorelines Ancient Shoreline Old Shoreline Recent Shoreline
  • 35. April 16, 2011 Swallow
  • 36. Tufas used to be underwater, they are made up of calcium, carbonate and lime, which were formed when fresh water and salt water meet. It also shows where streams used to meet the lake. April 16, 2011 Tufa
  • 37. North America’s newest mountain range. It was made up by volcanoes, in which there are 110 in the area. April 16,2011 Mono Crater
  • 38. April 16, 2011 Convict Lake
  • 39. Convict Lake got its name when convicts were found after they had escaped from prison and later were hung by authorities in 1871. April 16, 2011 Convict Lake Oldest Rock Formation Lateral Moraine Convict Lake
  • 40. A terminal is the sediment that was moved from it place by glaciers. April 16, 2011 Terminal Terminal
  • 41. April 16, 2011 Owens River
  • 42. This benchmark is found next to the Owens River, near Bishop, California. April 16, 2011 Benchmark
  • 43. Swallow nests are found underneath this bridge above the Owens River. April 16, 2011 Owens River with Swallows nests Swallows Nests Owens River
  • 44. Bristlecone trees are about 4500 years old and are the oldest living trees in the world. April 16, 2011 Inyo-White Mountains with Bristlecones Bristlecones Inyo-White Mountains
  • 45. April 17, 2011 Eastern California Museum
  • 46. I chose this picture because it is part of a model of what a Japanese Internment camp would look like. Now not very many are still standing. April 17, 2011 Internment Camp
  • 47. April 17, 2011 Manzanar
  • 48. Manzanar was one of ten labor camps in which people of Japanese decent were sent during World War II. About 110,000 men, women, and children lived here. April 17, 2011 Manzanar War Relocation Center
  • 49. This is part of what is left of Manzanar. Most of its buildings and artifacts were removed from this camp and were used to build other buildings in the neighboring town, or sent to museums. April 17, 2011 Manzanar Area
  • 51. Solar Power Plant April 2, 2011
  • 52. Koehn Lake Desert Playa April 2, 2011
  • 53. Doppler Radar Towers are used to measure wind. Doppler Radar Tower April 2, 2011
  • 54. Near Red Mountain, Rand Mining District. Mine Tailings
  • 55. April 2, 2011 Garlock Fault
  • 56. April 2, 2011 California Aqueduct
  • 57. Mojave Desert Wildflowers April 2, 2011
  • 58. April 15, 2011 Cucamonga Alluvial Fan Cucamonga Alluvial Fan
  • 59. Desert Vegetation Joshua Tree Creosote April 15, 2011
  • 60. April 15, 2011 Desert Vegetation Burroweed Grass
  • 61. April 15, 2011 Owens Dry Lake Owens Dry Lake
  • 62. April 15, 2011 SETI Towers