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  • Aerial Photography with a drone. Elevated view of the eroded sandstone mountains on the shore of the Dead Sea, Israel.
    BT_f_Dead-Sea_DJI_0028.jpg
  • Aerial Photography with a drone. Elevated view of the eroded sandstone mountains on the shore of the Dead Sea, Israel.
    DN_Drone-Dead-Sea_0011-1.jpg
  • Aerial Photography with a drone. Elevated view of the eroded sandstone mountains on the shore of the Dead Sea, Israel.
    DN_Drone-Dead-Sea_0016-1.jpg
  • Aerial Photography with a drone. Elevated view of the eroded sandstone mountains on the shore of the Dead Sea, Israel.
    DN_Drone-Dead-Sea_0004.jpg
  • Aerial Photography with a drone. Elevated view of the eroded sandstone mountains on the shore of the Dead Sea, Israel.
    BT_f_Dead-Sea_DJI_0022.jpg
  • Aerial Photography with a drone. Elevated view of the eroded sandstone mountains on the shore of the Dead Sea, Israel.
    DN_Drone-Dead-Sea_0015-1.jpg
  • Aerial Photography with a drone. Elevated view of the eroded sandstone mountains on the shore of the Dead Sea, Israel.
    BT_f_Dead-Sea_DJI_0032.jpg
  • Aerial Photography with a drone. Elevated view of the eroded sandstone mountains on the shore of the Dead Sea, Israel.
    DN_Drone-Dead-Sea_0010-2.jpg
  • Aerial Photography with a drone. Elevated view of the eroded sandstone mountains on the shore of the Dead Sea, Israel.
    DN_Drone-Dead-Sea_0009-2.jpg
  • Aerial Photography with a drone. Elevated view of the eroded sandstone mountains on the shore of the Dead Sea, Israel.
    DN_Drone-Dead-Sea_0006-1.jpg
  • Israel, Sodom, near the southern part of the Dead Sea, Eroded rock
    AMS_f_Desert_philosophersrock.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_27.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_24.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_La-Digue-Seychelles_44.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_31.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_21.jpg
  • Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    VA_f_Dead-sea_280.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_La-Digue-Seychelles_45.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_La-Digue-Seychelles_43.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Seychelles-rocky-shore_34.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_32.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_29.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_28.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_30.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_25.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_23.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_20.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_La-Digue-Seychelles_42.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Seychelles-rocky-shore_35.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_26.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_22.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_19.jpg
  • Eroded Red Rock formations in the Canon Del Inca, Tupiza Chichas Range, Bolivia
    JK_Bolivia_0547.jpg
  • Eroded granite. The action of waves over countless millennia has shaped the hard granite into these sculpted formations. This is the tropical island of La Digue, part of the Seychelles islands of the Indian Ocean. The Seychelles islands formed some 200 million years ago when India and Madagascar split off from Africa. They are unique as the only granite islands in the world, as well as being the oldest islands in the world. Many such sculpted granite boulders and outcrops are found along the beaches of the Seychelles.
    BT_Erosion_33.jpg
  • Israel, Sodom, near the southern part of the Dead Sea, Eroded rock
    SL_0903_A_shay_best_1_fs.jpg
  • Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    VA_casui-dunes_300.jpg
  • Eroded coastal cliff. Photographed on the Mediterranean coast, Israel
    BT_Coastal-Plains_IA8A7165.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_DSCF7319.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_DSCF7314.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_DSCF7324-Pano.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_DSCF7316.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_DAN0293.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_0018_1897-Pano.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_DSCF7311-Pano.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_DSCF7329-Pano.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_P1300280.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_DSCF7332.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_DSCF7327.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_0029_1908.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_0028_1907.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_P1300279.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_7106_6720.jpg
  • Israel, Dead Sea, Ein Gedi national park the eroded marl stone cliff overlooking the stream
    VA_f_Nahal-David_DSC09503.jpg
  • Israel, Dead Sea, Ein Gedi national park the eroded marl stone cliff overlooking the stream
    VA_f_Nahal-David_DSC09504.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    VA_f_Dead-Sea_DSC09757.jpg
  • Antelope Canyon, Arizona, USA, eroded Sandstone Rock Formations
    GE_f_Antelope-Canyon_1455.jpg
  • Antelope Canyon, Arizona, USA, eroded Sandstone Rock Formations
    DN_Antelope-Canyon_4.jpg
  • Antelope Canyon, Arizona, USA, eroded Sandstone Rock Formations
    DN_Antelope-Canyon_3.jpg
  • Madagascar, Ankarana Special Reserve. Tsingy - eroded limestone
    RH_Madagascar_09587.jpg
  • Madagascar, Ankarana Special Reserve. Tsingy - eroded limestone
    RH_Madagascar_09564.jpg
  • Israel, Dead Sea, Ein Gedi national park the eroded marl stone cliff overlooking the stream
    VA_f_Nahal-David_DSC09505.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    VA_f_Dead-Sea_DSC09771.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    VA_f_Dead-Sea_DSC09756.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_dscg1124.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    DN_f_Dead-Sea_dscg1122.jpg
  • Madagascar, Tsingy de Bemaraha Strict Nature Reserve - eroded Karst limestone
    GF_Madagascar_8244.jpg
  • Madagascar, Tsingy de Bemaraha Strict Nature Reserve - eroded Karst limestone
    GF_Madagascar_8239.jpg
  • Antelope Canyon, Arizona, USA, eroded Sandstone Rock Formations
    GE_f_Antelope-Canyon_1478.jpg
  • Antelope Canyon, Arizona, USA, eroded Sandstone Rock Formations
    GE_f_Antelope-Canyon_1468.jpg
  • Antelope Canyon, Arizona, USA, eroded Sandstone Rock Formations
    GE_f_Antelope-Canyon_1453.jpg
  • Antelope Canyon, Arizona, USA, eroded Sandstone Rock Formations
    GE_f_Antelope-Canyon_1451.jpg
  • Madagascar, Ankarana Special Reserve. Tsingy - eroded limestone
    RH_Madagascar_09642.jpg
  • Madagascar, Ankarana Special Reserve. Tsingy - eroded limestone
    RH_Madagascar_09582.jpg
  • Madagascar, Ankarana Special Reserve. Tsingy - eroded limestone  Large base of an Adenia tree
    RH_Madagascar_09572.jpg
  • Madagascar, Ankarana Special Reserve. Tsingy - eroded limestone
    RH_Madagascar_09565.jpg
  • Madagascar, Ankarana Special Reserve. Tsingy - eroded limestone
    RH_Madagascar_09560.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    VA_f_Dead-Sea_DSC09763.jpg
  • Madagascar, Tsingy de Bemaraha Strict Nature Reserve - eroded Karst limestone
    GF_Madagascar_8243.jpg
  • Madagascar, Tsingy de Bemaraha Strict Nature Reserve - eroded Karst limestone
    GF_Madagascar_8242.jpg
  • Madagascar, Ankarana Special Reserve. Tsingy - eroded limestone
    GF_Madagascar_8237.jpg
  • Antelope Canyon, Arizona, USA, eroded Sandstone Rock Formations
    GE_f_Antelope-Canyon_1452.jpg
  • Antelope Canyon, Arizona, USA, eroded Sandstone Rock Formations
    DN_Antelope-Canyon_2.jpg
  • Antelope Canyon, Arizona, USA, eroded Sandstone Rock Formations
    DN_Antelope-Canyon_1.jpg
  • Marl stone formations. Eroded cliffs made of marl. Marl is a calcium carbonate-rich, mudstone formed from sedimentary deposits. Photographed in Israel, Dead Sea region
    AM_Dead-Sea_5870.jpg
  • Madagascar, Ankarana Special Reserve. Tsingy - eroded limestone
    RH_Madagascar_09606.jpg
  • Madagascar, Ankarana Special Reserve. Tsingy - eroded limestone
    RH_Madagascar_09585.jpg
  • Madagascar, Ankarana Special Reserve. Tsingy - eroded limestone
    RH_Madagascar_09566.jpg
  • The Arch, Timna Valley, Arava, Israel. The Timna Natural and Historic park is located in the southwestern Arava, some 30 km. north of the Gulf of Eilat.
    VA_f_Timna_DSC08718.jpg
  • Solomon's Pillars, Timna Valley, Arava, Israel. The Timna Natural and Historic park is located in the southwestern Arava, some 30 km. north of the Gulf of Eilat.
    VA_f_Timna_DSC01202.jpg
  • The Arch, Timna Valley, Arava, Israel. The Timna Natural and Historic park is located in the southwestern Arava, some 30 km. north of the Gulf of Eilat.
    VA_f_Timna_DSC01159.jpg
  • Solomon's Pillars, Timna Valley, Arava, Israel
    BT_Timna_C7T9942.jpg
  • Solomon's Pillars, Timna Valley, Arava, Israel. The Timna Natural and Historic park is located in the southwestern Arava, some 30 km. north of the Gulf of Eilat.
    VA_f_Timna_DSC08834.jpg
  • Solomon's Pillars, Timna Valley, Arava, Israel. The Timna Natural and Historic park is located in the southwestern Arava, some 30 km. north of the Gulf of Eilat.
    VA_f_Timna_DSC08813.jpg
  • The Arch, Timna Valley, Arava, Israel. The Timna Natural and Historic park is located in the southwestern Arava, some 30 km. north of the Gulf of Eilat.
    VA_f_Timna_DSC08746.jpg
  • Landscape Timna Valley, Arava, Israel. The Timna Natural and Historic park is located in the southwestern Arava, some 30 km. north of the Gulf of Eilat.
    VA_f_Timna_DSC08734.jpg
  • The Arch, Timna Valley, Arava, Israel. The Timna Natural and Historic park is located in the southwestern Arava, some 30 km. north of the Gulf of Eilat.
    VA_f_Timna_DSC08717.jpg
  • The mushroom rock at Timna valley. Natural Rock formations, Timna natural and historic park, Israel, The Timna Valley is located in the southwestern Arava, some 30 km. north of the Gulf of Eilat.Photographed at Timna park, Israel.
    VA_f_Timna_DSC08693.jpg
  • Landscape Timna Valley, Arava, Israel. The Timna Natural and Historic park is located in the southwestern Arava, some 30 km. north of the Gulf of Eilat.
    VA_f_Timna_DSC08643.jpg
  • The mushroom rock at Timna valley. Natural Rock formations, Timna natural and historic park, Israel, The Timna Valley is located in the southwestern Arava, some 30 km. north of the Gulf of Eilat.Photographed at Timna park, Israel.
    VA_f_Timna_DSC08637.jpg
  • The mushroom rock at Timna valley. Natural Rock formations, Timna natural and historic park, Israel, The Timna Valley is located in the southwestern Arava, some 30 km. north of the Gulf of Eilat.Photographed at Timna park, Israel.
    VA_f_Timna_DSC08626.jpg
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