Gaviota State Park Photo
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Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara
Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara. Gaviota State Park Photo.
Image ID: 14892  
Location: Gaviota State Beach, Santa Barbara, California, USA
 		 Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara. Gaviota State Park Picture.
Image ID: 14893  
Location: Gaviota State Beach, Santa Barbara, California, USA
 		 Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara. Stock Photography of Gaviota State Park.
Image ID: 14894  
Location: Gaviota State Beach, Santa Barbara, California, USA
 
Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara
Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara. Photograph of Gaviota State Park.
Image ID: 14895  
Location: Gaviota State Beach, Santa Barbara, California, USA
 		 Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara. Gaviota State Park Photos.
Image ID: 14896  
Location: Gaviota State Beach, Santa Barbara, California, USA
 		 Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara. Gaviota State Park Image.
Image ID: 14897  
Location: Gaviota State Beach, Santa Barbara, California, USA
 
Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara
Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara. Professional stock photos of Gaviota State Park.
Image ID: 14898  
Location: Gaviota State Beach, Santa Barbara, California, USA
 		 Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara. Pictures of Gaviota State Park.
Image ID: 14899  
Location: Gaviota State Beach, Santa Barbara, California, USA
 
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Location  >  Protected Threatened and Significant Places  >  State Parks  >  Gaviota State Park
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Updated: February 10, 2012