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Field Lab Assignment Part I Arthur Nelson Geol 1- C01 12/5/10
Where I Found My Samples To look for my samples I went out to the Kings River in and around Lemoore, CA.
The Kings River starts in the Sierra Nevada, having three forks. The forks get back together in Fresno Country, where it is rapids. The water from the river flows to a dam in the foothills, and then splits six miles north of Lemoore into two more forks which join five miles west of Lemoore. The water then flows through an artificial channel into the Tulare Lake bed. In the Hanford area it has been that the depths to groundwater are increasing. There are many dams along the Kings River, because of the rise in hydroelectric power. In the San Joaquin Valley the water also helps to provide irrigation water.
Conglomerate A conglomerate rock consists of many smaller rocks cemented together by a fine-grained matrix. It is a sedimentary rock. The fragments are rounded and the clasts, or pieces of rock in the conglomerate, are larger than sand.
Jasper This rock which I found I believe to be Jasper, but I’m not completely sure about it. Jasper gets its red color from iron oxide, and it is a sedimentary rock. It has a smooth surface and is sometimes polished in order to be used for decoration.
Potassium Feldspar Feldspar is the most common mineral group because it can form under a wide range of temperatures and pressures. This rock has two planes of cleavage meeting at or near 90 degree angles. There are two different feldspar 				     	     structures, potassium and 			      plagioclase. Potassium is 				      either light cream, salmon 			      pink, or bluish-green.
Gneiss Gneiss rocks are medium  to coarse foliated. They  are developed under high temperature and pressure conditions. The gneiss  rocks are largely recrystallized, but do not have large quantities of many minerals. They are metamorphed igneous rocks.
Quartz Monozonite This is an igneous rock that is intrusive. There is a lot of quartz present in the quartz monozonite, and biotite and hornblende make it darker. Despite having the  word Quartz in it’s  name, even granite has more quartz in it.

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Field lab assignment part i

  • 1. Field Lab Assignment Part I Arthur Nelson Geol 1- C01 12/5/10
  • 2. Where I Found My Samples To look for my samples I went out to the Kings River in and around Lemoore, CA.
  • 3. The Kings River starts in the Sierra Nevada, having three forks. The forks get back together in Fresno Country, where it is rapids. The water from the river flows to a dam in the foothills, and then splits six miles north of Lemoore into two more forks which join five miles west of Lemoore. The water then flows through an artificial channel into the Tulare Lake bed. In the Hanford area it has been that the depths to groundwater are increasing. There are many dams along the Kings River, because of the rise in hydroelectric power. In the San Joaquin Valley the water also helps to provide irrigation water.
  • 4. Conglomerate A conglomerate rock consists of many smaller rocks cemented together by a fine-grained matrix. It is a sedimentary rock. The fragments are rounded and the clasts, or pieces of rock in the conglomerate, are larger than sand.
  • 5. Jasper This rock which I found I believe to be Jasper, but I’m not completely sure about it. Jasper gets its red color from iron oxide, and it is a sedimentary rock. It has a smooth surface and is sometimes polished in order to be used for decoration.
  • 6. Potassium Feldspar Feldspar is the most common mineral group because it can form under a wide range of temperatures and pressures. This rock has two planes of cleavage meeting at or near 90 degree angles. There are two different feldspar structures, potassium and plagioclase. Potassium is either light cream, salmon pink, or bluish-green.
  • 7. Gneiss Gneiss rocks are medium to coarse foliated. They are developed under high temperature and pressure conditions. The gneiss rocks are largely recrystallized, but do not have large quantities of many minerals. They are metamorphed igneous rocks.
  • 8. Quartz Monozonite This is an igneous rock that is intrusive. There is a lot of quartz present in the quartz monozonite, and biotite and hornblende make it darker. Despite having the word Quartz in it’s name, even granite has more quartz in it.