Stock Photos of Santa Barbara

Common dolphin at the edge of the ocean, Delphinus delphis, Santa Barbara, California
Common dolphin at the edge of the ocean.
Species: Common dolphin, Delphinus delphis
Location: Santa Barbara, California
Image ID: 27017  
Common dolphin leaping from the ocean, Delphinus delphis, Santa Barbara, California
Common dolphin leaping from the ocean.
Species: Common dolphin, Delphinus delphis
Location: Santa Barbara, California
Image ID: 27018  
Drift kelp has washed ashore on a sandy California beach.  Winter brings large surf and increased wave energy which often rips giant kelp from the ocean bottom, so that it floats down current, often washing ashore, Macrocystis pyrifera, Santa Barbara
Drift kelp has washed ashore on a sandy California beach. Winter brings large surf and increased wave energy which often rips giant kelp from the ocean bottom, so that it floats down current, often washing ashore.
Species: Giant kelp, Macrocystis pyrifera
Location: Santa Barbara, California
Image ID: 14884  
The Santa Barbara Mission.  Established in 1786, Mission Santa Barbara was the tenth of the California missions to be founded by the Spanish Franciscans.  Santa Barbara
The Santa Barbara Mission. Established in 1786, Mission Santa Barbara was the tenth of the California missions to be founded by the Spanish Franciscans. Santa Barbara.
Location: Santa Barbara Mission, California
Image ID: 14885  
The Santa Barbara Mission.  Established in 1786, Mission Santa Barbara was the tenth of the California missions to be founded by the Spanish Franciscans.  Santa Barbara
The Santa Barbara Mission. Established in 1786, Mission Santa Barbara was the tenth of the California missions to be founded by the Spanish Franciscans. Santa Barbara.
Location: Santa Barbara Mission, California
Image ID: 14886  
The Santa Barbara Mission.  Established in 1786, Mission Santa Barbara was the tenth of the California missions to be founded by the Spanish Franciscans.  Santa Barbara
The Santa Barbara Mission. Established in 1786, Mission Santa Barbara was the tenth of the California missions to be founded by the Spanish Franciscans. Santa Barbara.
Location: Santa Barbara Mission, California
Image ID: 14887  
The Santa Barbara Mission.  Established in 1786, Mission Santa Barbara was the tenth of the California missions to be founded by the Spanish Franciscans.  Santa Barbara
The Santa Barbara Mission. Established in 1786, Mission Santa Barbara was the tenth of the California missions to be founded by the Spanish Franciscans. Santa Barbara.
Location: Santa Barbara Mission, California
Image ID: 14888  
The Ty Warner Sea Center, a part of the Santa Barbara Museum of Natural History, located on Stearns Wharf, Santa Barbara Museum of History
The Ty Warner Sea Center, a part of the Santa Barbara Museum of Natural History, located on Stearns Wharf.
Location: Santa Barbara Museum of History, California
Image ID: 14889  
The Ty Warner Sea Center, a part of the Santa Barbara Museum of Natural History, located on Stearns Wharf, Santa Barbara Museum of History
The Ty Warner Sea Center, a part of the Santa Barbara Museum of Natural History, located on Stearns Wharf.
Location: Santa Barbara Museum of History, California
Image ID: 14890  
Inside of the parish of the Santa Barbara Mission.  Established in 1786, Mission Santa Barbara was the tenth of the California missions to be founded by the Spanish Franciscans.  Santa Barbara
Inside of the parish of the Santa Barbara Mission. Established in 1786, Mission Santa Barbara was the tenth of the California missions to be founded by the Spanish Franciscans. Santa Barbara.
Location: Santa Barbara Mission, California
Image ID: 14891  
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.
Location: Gaviota State Beach, Santa Barbara, California
Image ID: 14892  
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.
Location: Gaviota State Beach, Santa Barbara, California
Image ID: 14893  
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.
Location: Gaviota State Beach, Santa Barbara, California
Image ID: 14894  
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.
Location: Gaviota State Beach, Santa Barbara, California
Image ID: 14895  
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.
Location: Gaviota State Beach, Santa Barbara, California
Image ID: 14896  
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.
Location: Gaviota State Beach, Santa Barbara, California
Image ID: 14897  
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.
Location: Gaviota State Beach, Santa Barbara, California
Image ID: 14898  
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.
Location: Gaviota State Beach, Santa Barbara, California
Image ID: 14899  
Drift kelp has washed ashore on a sandy California beach.  Winter brings large surf and increased wave energy which often rips giant kelp from the ocean bottom, so that it floats down current, often washing ashore, Macrocystis pyrifera, Santa Barbara
Drift kelp has washed ashore on a sandy California beach. Winter brings large surf and increased wave energy which often rips giant kelp from the ocean bottom, so that it floats down current, often washing ashore.
Species: Giant kelp, Macrocystis pyrifera
Location: Santa Barbara, California
Image ID: 14883