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Field Lab PT 1/Rock Identification,[object Object],By: Jean Reyes,[object Object]
Location and background,[object Object],I have chosen a certain number of rock types that I have found near my job location. I have chosen these rocks by color, shape, crystal structure and, geographic location.,[object Object],Although these rocks are different, most should have similar historical background as they are from the same area.,[object Object],The rocks I have chosen are from a coastal area located near San Miguel, C.A. at Camp Roberts Military Training Center near the Santa Lucia Mountains, where I am currently employed.,[object Object]
   Location/Background continued…,[object Object],Camp Roberts is located near the Salinas River between Monterey and San Luis Obispo Counties.,[object Object],It is named after Harold W. Roberts, a World War 2 medal of honor recipient.,[object Object],It’s surrounded by the unincorporated communities of San Miguel, Heritage Ranch (Lake Nacimiento), and Bradley. Its closest incorporated city is Paso Robles, 12 miles south on HWY 101.,[object Object]
Location/background continued..,[object Object]
	Santa lucia mountains,[object Object],The rock of the Santa Lucia's is dominated by the granitic basement of the Salinian Block, between the San Andreas Fault and Sur-Nacimiento Fault. According to plate-tectonic theory, the core of the Salinian block formed as part of the same batholiths which forms the core of the Sierra Nevada Mountains and the Peninsular ranges of Baja California. It was broken off the North American plate and transported north by the action of the San Andreas fault from an original position. It is predominantly Mesozoic granitic and pre-Cretaceous metamorphic rock. There is some Cretaceous sedimentary rock of the Great Valley Sequence, considerable Miocene marine sediments, and some other Tertiary sediments. Units west of the Sur-Nacimiento fault are dominated by rocks of the Franciscan Assemblage.,[object Object]
	    Granite/granitic,[object Object],-Identified to be of igneous origin,[object Object],-Phaneritic in texture,[object Object],-Large crystal structure,[object Object],-Felsic composition,[object Object],-Intrusive (because of the coarse-grained texture).,[object Object],-presumed to be light in silicates as granite contains only 10% dark silicates.,[object Object]
	      Quartz/quartzite		   Metamorphic,[object Object],Identified to be of metamorphic origin.,[object Object], white with reddish/pinkish stains.,[object Object],Non-foliated/Porphyritic texture,[object Object],Medium-coarse grain,[object Object],Felsic composition,[object Object],Parent rock-Quartz sandstone,[object Object]
		Igneous/granite,[object Object],Identified as Igneous in origin,[object Object],Looks to be Pyroclastic in texture,[object Object], Intrusive (coarse grain),[object Object],Pink/reddish in color,[object Object],Mafic (Basaltic)/Gabbro composition,[object Object]
	Other Rock variances,[object Object]
		Possibilities/conclusion….	,[object Object],Much of the outlying rock families in this immediate area seem to be very consistent with the Metamorphic/Igneous families.,[object Object],A solid amount of this area does contain sediment and sedimentary rock.,[object Object],Most of my findings and rock samples are not consistent with the sedimentary history that is suggested through out this area.,[object Object],Perhaps Metamorphism and the metamorphic rock cyclic processes has taken over within this area over the past century or longer.,[object Object]
Field Lab pt: 2Field Observations,[object Object],by: Jean Reyes,[object Object]
		  Salinas river,[object Object],Located in central San Luis Obispo County,[object Object],Flows parallel to the Santa Lucia Mountains,[object Object],Elevation-2,400 ft,[object Object],Mouth-Monterey Bay,[object Object],Length-175 Miles (282 km),[object Object],Basin-4,160 sq miles,[object Object]
		 Erosion,[object Object],Because of its periodic dry climate and dry river bottom at times during the summer, the Salinas river bed endures harsh erosion.,[object Object],During the summer months the Salinas river dries up. In the winter, during rain and flood seasons, heavy water and strong currents break down the river bottom.,[object Object],-this picture shows a prime example of erosion and the weathering process that occurs.,[object Object]
	     Bridges/railroad,[object Object],Built and developed during WW2 to transport troops to and from Camp Roberts Military Training Center.,[object Object],Operated by Southern Pacific Railroad Transport,[object Object],No longer in operation (derailed after the Korean war),[object Object]
       Nacimiento Dam Spillway,[object Object],Nacimiento River Dam was constructed in 1961.,[object Object],Built by the Monterey County Water Authority for flood control and water irrigation.,[object Object],Created Lake Nacimiento which is now used by people for recreational purposes.,[object Object],It is a 210 ft earth fill dam.,[object Object]
		 Nacimiento continued…,[object Object],Nacimiento,[object Object],Nacimiento Dam Spillway has been undergoing extensive repair and modification operations since 2008.,[object Object],Purpose of modifications is to ensure safety regulations and to improve release maneuvers incase of large floods.,[object Object]

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Field lab pt 1

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