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  • Scenic of Pinnacle Rock<br />
Bartolome Island<br />
Galapagos<br />
Ecuador, South America
    20161128_Pinnacle_Rock_Panorama1.tif
  • Scenic of Pinnacle Rock<br />
Bartolome Island<br />
Galapagos<br />
Ecuador, South America
    20161128_Scenic_of_Pinnacle_Rock_40.tif
  • Scenic of Pinnacle Rock<br />
Bartolome Island<br />
Galapagos<br />
Ecuador, South America
    20161128_Scenic_of_Pinnacle_Rock_29.tif
  • Lava on Sullivan Bay<br />
a recent (1897) pahoehoe lava flow<br />
Sullivan Bay <br />
Santiago <br />
Pinnacle Rock and Bartolome Island in back<br />
Galapagos<br />
Ecuador, South America
    20161212_Sullivan_Bay_&_Pinnacle_Roc...jpg
  • Pinnacle Rock<br />
Bartolome Island<br />
Galapagos<br />
Ecuador, South America
    20160617_Pinnacle_Rock_215.jpg
  • Lava on Sullivan Bay<br />
a recent (1897) pahoehoe lava flow<br />
Sullivan Bay <br />
Santiago <br />
Pinnacle Rock and Bartolome Island in back<br />
Galapagos<br />
Ecuador, South America
    20161212_Sullivan_Bay_&_Pinnacle_Roc...tif
  • Scenic of Pinnacle Rock<br />
Bartolome Island<br />
Galapagos<br />
Ecuador, South America
    20161212_Scenic_of_Pinnacle_Rock_2.tif
  • Bartolome Island<br />
GALAPAGOS ISLANDS, ECUADOR.  South America
    1064472 Bartolome Island.tif
  • Tsingy or Limestone pinnacles formed by erosion. Ankarana Special Reserve. Northern MADAGASCAR<br />
During the Triassic (240-210Ma) the landscape of the island was uplifted and terrestrial gravels and sands were deposited. Then major marine transgression followed, and from this time, until after the demise of the dinosaurs fossiliferous marine limestone sedimentation dominated. These sediments today make up the Tsingy landscape of Madagascr.
    MA1139_Tsingy.tif
  • Tsingy or Limestone pinnacles formed by erosion. Ankarana Special Reserve. Northern MADAGASCAR<br />
During the Triassic (240-210Ma) the landscape of the island was uplifted and terrestrial gravels and sands were deposited. Then major marine transgression followed, and from this time, until after the demise of the dinosaurs fossiliferous marine limestone sedimentation dominated. These sediments today make up the Tsingy landscape of Madagascr.
    MA1138_Tsingy.tif
  • Tsingy or Limestone pinnacles formed by erosion. Ankarana Special Reserve. Northern MADAGASCAR<br />
During the Triassic (240-210Ma) the landscape of the island was uplifted and terrestrial gravels and sands were deposited. Then major marine transgression followed, and from this time, until after the demise of the dinosaurs fossiliferous marine limestone sedimentation dominated. These sediments today make up the Tsingy landscape of Madagascr.
    MA815_Tsingy.tif
  • King Vulture at Roost<br />
Sarcoramphus papa<br />
in Caatinga Habitat.  Bahia.  NE BRAZIL  South America
    113663 King Vulture at Roost.tif
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