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    Landscape of the Tabernas Desert, Andalusia (Spain). An ancient Miocene sedimentary basin (- 8Ma) at the foot of the Sierra Nevada. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600325JPG

    Landscape of the Tabernas Desert, Andalusia (Spain). An ancient

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Landscape of the Tabernas Desert, Andalusia (Spain). An ancient Miocene sedimentary basin (- 8Ma) at the foot of the Sierra Nevada. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Landscape of the Tabernas Desert, Andalusia (Spain). An ancient Miocene sedimentary basin (- 8Ma) at the foot of the Sierra Nevada. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600324JPG

    Landscape of the Tabernas Desert, Andalusia (Spain). An ancient Miocene sedimentary basin (- 8Ma) at the foot of the Sierra Nevada. The arid climate

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Landscape of the Tabernas Desert, Andalusia (Spain). An ancient Miocene sedimentary basin (- 8Ma) at the foot of the Sierra Nevada. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600323JPG

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600322JPG

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600321JPG

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600320JPG

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Flysch in the Tabernas Desert, Andalusia (Spain). Alternating sandstones and marls deposited in the Miocene (- 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600319JPG

    Flysch in the Tabernas Desert, Andalusia (Spain). Alternating

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Flysch in the Tabernas Desert, Andalusia (Spain). Alternating sandstones and marls deposited in the Miocene (- 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Flysch in the Tabernas Desert, Andalusia (Spain). Alternating sandstones and marls deposited in the Miocene (- 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600318JPG

    Flysch in the Tabernas Desert, Andalusia (Spain). Alternating

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Flysch in the Tabernas Desert, Andalusia (Spain). Alternating sandstones and marls deposited in the Miocene (- 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Seismites in the Granada Geopark, Spain. Galera and Castilléjar seismites: seismic waves transform sediments into a kind of quicksand. The water in the sediment's pores is expelled, separating the grains and transforming the material into a viscous fluid (liquefaction) that congeals into thousands of concentric structures throughout the sedimentary stratum.

    RM2600317JPG

    Seismites in the Granada Geopark, Spain. Galera and Castilléjar seismites: seismic waves transform sediments into a kind of quicksand. The water in

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Seismites in the Granada Geopark, Spain. Galera and Castilléjar seismites: seismic waves transform sediments into a kind of quicksand. The water in the sediment's pores is expelled, separating the grains and transforming the material into a viscous fluid (liquefaction) that congeals into thousands of concentric structures throughout the sedimentary stratum.

    Seismites in the Granada Geopark, Spain. Galera and Castilléjar seismites: seismic waves transform sediments into a kind of quicksand. The water in the sediment's pores is expelled, separating the grains and transforming the material into a viscous fluid (liquefaction) that congeals into thousands of concentric structures throughout the sedimentary stratum.

    RM2600316JPG

    Seismites in the Granada Geopark, Spain. Galera and Castilléjar

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Seismites in the Granada Geopark, Spain. Galera and Castilléjar seismites: seismic waves transform sediments into a kind of quicksand. The water in the sediment's pores is expelled, separating the grains and transforming the material into a viscous fluid (liquefaction) that congeals into thousands of concentric structures throughout the sedimentary stratum.

    Seismites in the Granada Geopark, Spain. Galera and Castilléjar seismites: seismic waves transform sediments into a kind of quicksand. The water in the sediment's pores is expelled, separating the grains and transforming the material into a viscous fluid (liquefaction) that congeals into thousands of concentric structures throughout the sedimentary stratum.

    RM2600315JPG

    Seismites in the Granada Geopark, Spain. Galera and Castilléjar

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Seismites in the Granada Geopark, Spain. Galera and Castilléjar seismites: seismic waves transform sediments into a kind of quicksand. The water in the sediment's pores is expelled, separating the grains and transforming the material into a viscous fluid (liquefaction) that congeals into thousands of concentric structures throughout the sedimentary stratum.

    Orange trees in Andalusia. Costa Tropical, between Malaga and Almeria - Climate favorable to the cultivation of many semi-tropical species such as orange, lemon and avocado trees. Spain

    RM2600314JPG

    Orange trees in Andalusia. Costa Tropical, between Malaga and Almeria - Climate favorable to the cultivation of many semi-tropical species such as

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Orange trees in Andalusia. Costa Tropical, between Malaga and Almeria - Climate favorable to the cultivation of many semi-tropical species such as orange, lemon and avocado trees. Spain

    Olive trees in the middle of badlands in Andalusia. Badlands at the foot of the Mencal. Olive and almond trees are the main crops in this arid region. Guadix region - Granada Geopark - Spain

    RM2600313JPG

    Olive trees in the middle of badlands in Andalusia. Badlands at the foot of the Mencal. Olive and almond trees are the main crops in this arid region. Guadix region -

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Olive trees in the middle of badlands in Andalusia. Badlands at the foot of the Mencal. Olive and almond trees are the main crops in this arid region. Guadix region - Granada Geopark - Spain

    Sandstone densely covered with lichens in Spain. Saxicolous crustaceous lichens - Malaga region, Andalusia

    RM2600312JPG

    Sandstone densely covered with lichens in Spain. Saxicolous

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Sandstone densely covered with lichens in Spain. Saxicolous crustaceous lichens - Malaga region, Andalusia

    Sandstone densely covered with lichens in Spain. Saxicolous crustaceous lichens - Malaga region, Andalusia

    RM2600311JPG

    Sandstone densely covered with lichens in Spain. Saxicolous crustaceous lichens - Malaga region, Andalusia

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Sandstone densely covered with lichens in Spain. Saxicolous crustaceous lichens - Malaga region, Andalusia

    Lichens and gypsum macrocrystals from the Sorbas Karst in Andalusia. The Sorbas gypsum karst is unique in Europe. The aridity of the region, close to the Tabernas desert, means that layers of gypsum, carved out by erosion into karst like limestone, remain on the surface. This gypsum was formed when the Mediterranean dried up during the Messinian crisis in the Miocene (-6 Ma), leaving behind huge evaporite deposits.

    RM2600310JPG

    Lichens and gypsum macrocrystals from the Sorbas Karst in Andalusia. The Sorbas gypsum karst is unique in Europe. The aridity of the region, close to

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Lichens and gypsum macrocrystals from the Sorbas Karst in Andalusia. The Sorbas gypsum karst is unique in Europe. The aridity of the region, close to the Tabernas desert, means that layers of gypsum, carved out by erosion into karst like limestone, remain on the surface. This gypsum was formed when the Mediterranean dried up during the Messinian crisis in the Miocene (-6 Ma), leaving behind huge evaporite deposits.

    Lichens and gypsum macrocrystals from the Sorbas Karst in Andalusia. The Sorbas gypsum karst is unique in Europe. The aridity of the region, close to the Tabernas desert, means that layers of gypsum, carved out by erosion into karst like limestone, remain on the surface. This gypsum was formed when the Mediterranean dried up during the Messinian crisis in the Miocene (-6 Ma), leaving behind huge evaporite deposits.

    RM2600309JPG

    Lichens and gypsum macrocrystals from the Sorbas Karst in Andalusia. The Sorbas gypsum karst is unique in Europe. The aridity of the region, close to

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Lichens and gypsum macrocrystals from the Sorbas Karst in Andalusia. The Sorbas gypsum karst is unique in Europe. The aridity of the region, close to the Tabernas desert, means that layers of gypsum, carved out by erosion into karst like limestone, remain on the surface. This gypsum was formed when the Mediterranean dried up during the Messinian crisis in the Miocene (-6 Ma), leaving behind huge evaporite deposits.

    Lichens and gypsum macrocrystals from the Sorbas Karst in Andalusia. The Sorbas gypsum karst is unique in Europe. The aridity of the region, close to the Tabernas desert, means that layers of gypsum, carved out by erosion into karst like limestone, remain on the surface. This gypsum was formed when the Mediterranean dried up during the Messinian crisis in the Miocene (-6 Ma), leaving behind huge evaporite deposits.

    RM2600308JPG

    Lichens and gypsum macrocrystals from the Sorbas Karst in Andalusia. The Sorbas gypsum karst is unique in Europe. The aridity of the region, close to

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Lichens and gypsum macrocrystals from the Sorbas Karst in Andalusia. The Sorbas gypsum karst is unique in Europe. The aridity of the region, close to the Tabernas desert, means that layers of gypsum, carved out by erosion into karst like limestone, remain on the surface. This gypsum was formed when the Mediterranean dried up during the Messinian crisis in the Miocene (-6 Ma), leaving behind huge evaporite deposits.

    Clay and gypsum crystals in the Granada Geopark, Spain. Andalusia

    RM2600307JPG

    Clay and gypsum crystals in the Granada Geopark, Spain. Andalusia

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Clay and gypsum crystals in the Granada Geopark, Spain. Andalusia

    Rock engraving in a rock shelter in Andalusia. Las Piedras de Cabrera complex north of Malaga - Early Chalcolithic period, between 2600 and 2300 B.C. - Spain

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    Rock engraving in a rock shelter in Andalusia. Las Piedras de Cabrera complex north of Malaga - Early Chalcolithic period, between 2600 and 2300 B.C.

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Rock engraving in a rock shelter in Andalusia. Las Piedras de Cabrera complex north of Malaga - Early Chalcolithic period, between 2600 and 2300 B.C. - Spain

    Cynomorium scarlet, (Cynomorium coccineum ) in the Tabernas desert (Andalusia - Spain). Parasitic species of tamarix, salsola and limonium, appearing only at flowering as a dense spike inflorescence. An ancient Miocene sedimentary basin (- 8Ma) at the foot of the Sierra Nevada. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain. In the foreground, lichens of the Diploschistes genus cover the clay soil.

    RM2600305JPG

    Cynomorium scarlet, (Cynomorium coccineum ) in the Tabernas desert (Andalusia - Spain). Parasitic species of tamarix, salsola and limonium, appearing

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Cynomorium scarlet, (Cynomorium coccineum ) in the Tabernas desert (Andalusia - Spain). Parasitic species of tamarix, salsola and limonium, appearing only at flowering as a dense spike inflorescence. An ancient Miocene sedimentary basin (- 8Ma) at the foot of the Sierra Nevada. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain. In the foreground, lichens of the Diploschistes genus cover the clay soil.

    Dwarf doum palms in Cabo de Gata, Andalusia (Spain). Dwarf or doum palms (Chamaerops humilis), one of Europe's two native palms, indicative of the semi-arid Mediterranean vegetation zone. Cabo de Gata Natural Park / Geopark in Andalusia

    RM2600304JPG

    Dwarf doum palms in Cabo de Gata, Andalusia (Spain). Dwarf or doum palms (Chamaerops humilis), one of Europe's two native palms, indicative of the

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Dwarf doum palms in Cabo de Gata, Andalusia (Spain). Dwarf or doum palms (Chamaerops humilis), one of Europe's two native palms, indicative of the semi-arid Mediterranean vegetation zone. Cabo de Gata Natural Park / Geopark in Andalusia

    Dwarf doum palms in Cabo de Gata, Andalusia (Spain). Dwarf or doum palms (Chamaerops humilis), one of Europe's two native palms, indicative of the semi-arid Mediterranean vegetation zone. Cabo de Gata Natural Park / Geopark in Andalusia

    RM2600303JPG

    Dwarf doum palms in Cabo de Gata, Andalusia (Spain). Dwarf or doum palms (Chamaerops humilis), one of Europe's two native palms, indicative of the

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Dwarf doum palms in Cabo de Gata, Andalusia (Spain). Dwarf or doum palms (Chamaerops humilis), one of Europe's two native palms, indicative of the semi-arid Mediterranean vegetation zone. Cabo de Gata Natural Park / Geopark in Andalusia

    Wind-swept dune at Cabo de Gata in Andalusia. Huge crescent-shaped dune at Playa de Monsul - Cabo de Gata Geopark

    RM2600302JPG

    Wind-swept dune at Cabo de Gata in Andalusia. Huge crescent-shaped dune at Playa de Monsul - Cabo de Gata Geopark

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Wind-swept dune at Cabo de Gata in Andalusia. Huge crescent-shaped dune at Playa de Monsul - Cabo de Gata Geopark

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    RM2600301JPG

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance,

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    RM2600300JPG

    Andesite columns in the Cabo de Gata Geopark, Andalusia.

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    RM2600299JPG

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance,

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    White Ignimbrites from Cala Rajada, in the Cabo de Gata Geopark, Andalusia. Welded pumice and lapilli from pyroclastic flows (approx. 10 Ma). In the background, Cerro de la Vela Blanca and Arrecife del Dedo are formed of manganese-rich dark andesite. Cabo de Gata volcanic complex (Geopark)

    RM2600298JPG

    White Ignimbrites from Cala Rajada, in the Cabo de Gata Geopark, Andalusia. Welded pumice and lapilli from pyroclastic flows (approx. 10 Ma). In the

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    White Ignimbrites from Cala Rajada, in the Cabo de Gata Geopark, Andalusia. Welded pumice and lapilli from pyroclastic flows (approx. 10 Ma). In the background, Cerro de la Vela Blanca and Arrecife del Dedo are formed of manganese-rich dark andesite. Cabo de Gata volcanic complex (Geopark)

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    RM2600297JPG

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance,

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    RM2600296JPG

    Andesite columns in the Cabo de Gata Geopark, Andalusia.

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    RM2600295JPG

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance,

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    RM2600294JPG

    Andesite columns in the Cabo de Gata Geopark, Andalusia.

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    RM2600293JPG

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance,

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Andesite columns in the Cabo de Gata Geopark, Andalusia. Andesites with columnar disjunction in the Punta Baja dome. Basaltic organ-like appearance, but very different nature and formation, on the surface of a large dome. Cabo de Gata volcanic complex (Geopark)

    Calcarenite cliffs in the Cabo de Gata Geopark, Andalusia. Bioclastic deposits of around 6 Ma - Rodalquilar sector, Cabo de Gata Geopark, southern Spain

    RM2600292JPG

    Calcarenite cliffs in the Cabo de Gata Geopark, Andalusia. Bioclastic deposits of around 6 Ma - Rodalquilar sector, Cabo de Gata Geopark, southern

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Calcarenite cliffs in the Cabo de Gata Geopark, Andalusia. Bioclastic deposits of around 6 Ma - Rodalquilar sector, Cabo de Gata Geopark, southern Spain

    Calcarenite cliffs in the Cabo de Gata Geopark, Andalusia. Bioclastic deposits of around 6 Ma - Rodalquilar sector, Cabo de Gata Geopark, southern Spain

    RM2600291JPG

    Calcarenite cliffs in the Cabo de Gata Geopark, Andalusia. Bioclastic deposits of around 6 Ma - Rodalquilar sector, Cabo de Gata Geopark, southern

    © Jean-Philippe Delobelle / Biosphoto

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    2600291
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    © Jean-Philippe Delobelle / Biosphoto

    Calcarenite cliffs in the Cabo de Gata Geopark, Andalusia. Bioclastic deposits of around 6 Ma - Rodalquilar sector, Cabo de Gata Geopark, southern Spain

    White village on the edge of badlands in the Granada Geopark, Spain. Beas de Guadix. Alluvial deposits of late Miocene conglomerates and clays, eroded into spectacular badlands. Andalusia

    RM2600290JPG

    White village on the edge of badlands in the Granada Geopark, Spain. Beas de Guadix. Alluvial deposits of late Miocene conglomerates and clays,

    © Jean-Philippe Delobelle / Biosphoto

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    2600290
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    © Jean-Philippe Delobelle / Biosphoto

    White village on the edge of badlands in the Granada Geopark, Spain. Beas de Guadix. Alluvial deposits of late Miocene conglomerates and clays, eroded into spectacular badlands. Andalusia

    Badlands in the Granada Geopark, Spain. Beas de Guadix region. Alluvial deposits of late Miocene conglomerates and clays, eroded into spectacular badlands. Andalusia

    RM2600289JPG

    Badlands in the Granada Geopark, Spain. Beas de Guadix region. Alluvial deposits of late Miocene conglomerates and clays, eroded into spectacular

    © Jean-Philippe Delobelle / Biosphoto

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    2600289
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    © Jean-Philippe Delobelle / Biosphoto

    Badlands in the Granada Geopark, Spain. Beas de Guadix region. Alluvial deposits of late Miocene conglomerates and clays, eroded into spectacular badlands. Andalusia

    Badlands in the Granada Geopark, Spain. Gorafe region: alluvial deposits of late Miocene conglomerates and clays, eroded into spectacular badlands. Andalusia

    RM2600288JPG

    Badlands in the Granada Geopark, Spain. Gorafe region: alluvial deposits of late Miocene conglomerates and clays, eroded into spectacular badlands.

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Badlands in the Granada Geopark, Spain. Gorafe region: alluvial deposits of late Miocene conglomerates and clays, eroded into spectacular badlands. Andalusia

    Lemon tree and bench in the "white village" of Ojen, near Marbella. The famous white villages of Andalusia are a series of picturesque villages perched on the hills and mountains of the region, characterized by their whitewashed houses and narrow streets, and whose architecture is inherited from the Arab period.

    RM2600287JPG

    Lemon tree and bench in the "white village" of Ojen, near Marbella. The famous white villages of Andalusia are a series of picturesque villages

    © Jean-Philippe Delobelle / Biosphoto

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    2600287
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    © Jean-Philippe Delobelle / Biosphoto

    Lemon tree and bench in the "white village" of Ojen, near Marbella. The famous white villages of Andalusia are a series of picturesque villages perched on the hills and mountains of the region, characterized by their whitewashed houses and narrow streets, and whose architecture is inherited from the Arab period.

    Lemon tree and bench in the "white village" of Ojen, near Marbella. The famous white villages of Andalusia are a series of picturesque villages perched on the hills and mountains of the region, characterized by their whitewashed houses and narrow streets, and whose architecture is inherited from the Arab period.

    RM2600286JPG

    Lemon tree and bench in the "white village" of Ojen, near

    © Jean-Philippe Delobelle / Biosphoto

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    2600286
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    © Jean-Philippe Delobelle / Biosphoto

    Lemon tree and bench in the "white village" of Ojen, near Marbella. The famous white villages of Andalusia are a series of picturesque villages perched on the hills and mountains of the region, characterized by their whitewashed houses and narrow streets, and whose architecture is inherited from the Arab period.

    Lemon tree and bench in the "white village" of Ojen, near Marbella. The famous white villages of Andalusia are a series of picturesque villages perched on the hills and mountains of the region, characterized by their whitewashed houses and narrow streets, and whose architecture is inherited from the Arab period.

    RM2600285JPG

    Lemon tree and bench in the "white village" of Ojen, near Marbella. The famous white villages of Andalusia are a series of picturesque villages

    © Jean-Philippe Delobelle / Biosphoto

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    2600285
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    © Jean-Philippe Delobelle / Biosphoto

    Lemon tree and bench in the "white village" of Ojen, near Marbella. The famous white villages of Andalusia are a series of picturesque villages perched on the hills and mountains of the region, characterized by their whitewashed houses and narrow streets, and whose architecture is inherited from the Arab period.

    Almond trees in bloom in Andalusia. Guadix region - Granada Geopark - Spain

    RM2600284JPG

    Almond trees in bloom in Andalusia. Guadix region - Granada Geopark - Spain

    © Jean-Philippe Delobelle / Biosphoto

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    2600284
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    © Jean-Philippe Delobelle / Biosphoto

    Almond trees in bloom in Andalusia. Guadix region - Granada Geopark - Spain

    Almond trees in bloom in Andalusia. Guadix region - Granada Geopark - Spain

    RM2600283JPG

    Almond trees in bloom in Andalusia. Guadix region - Granada Geopark - Spain

    © Jean-Philippe Delobelle / Biosphoto

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    2600283
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    © Jean-Philippe Delobelle / Biosphoto

    Almond trees in bloom in Andalusia. Guadix region - Granada Geopark - Spain

    Almond trees in bloom in Andalusia. Guadix region - Granada Geopark - Spain

    RM2600282JPG

    Almond trees in bloom in Andalusia. Guadix region - Granada Geopark - Spain

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Almond trees in bloom in Andalusia. Guadix region - Granada Geopark - Spain

    Fields, almond blossoms and olive trees in Andalusia. Guadix region - Granada Geopark - Spain

    RM2600281JPG

    Fields, almond blossoms and olive trees in Andalusia. Guadix region - Granada Geopark - Spain

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Fields, almond blossoms and olive trees in Andalusia. Guadix region - Granada Geopark - Spain

    Almond trees in bloom in Andalusia. Guadix region - Granada Geopark - Spain

    RM2600280JPG

    Almond trees in bloom in Andalusia. Guadix region - Granada Geopark - Spain

    © Jean-Philippe Delobelle / Biosphoto

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    2600280
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    © Jean-Philippe Delobelle / Biosphoto

    Almond trees in bloom in Andalusia. Guadix region - Granada Geopark - Spain

    White villages of the Alpujarras in Andalusia's Sierra Nevada. Capileira, 1,436 m above sea level on the southern slopes of the Sierra Nevada. On the right, the village of Bubion. Spain

    RM2600279JPG

    White villages of the Alpujarras in Andalusia's Sierra Nevada. Capileira, 1,436 m above sea level on the southern slopes of the Sierra Nevada. On the

    © Jean-Philippe Delobelle / Biosphoto

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    2600279
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    © Jean-Philippe Delobelle / Biosphoto

    White villages of the Alpujarras in Andalusia's Sierra Nevada. Capileira, 1,436 m above sea level on the southern slopes of the Sierra Nevada. On the right, the village of Bubion. Spain

    Galleries of bark beetle larvae (Ips typographus) under the bark of a spruce tree in the French Alps. Close-up Photographer of the Year (CUPOTY) - Intimate Landscape Winner - A Network of Life and Death

    RM2598553JPG

    Galleries of bark beetle larvae (Ips typographus) under the bark of a spruce tree in the French Alps. Close-up Photographer of the Year (CUPOTY) -

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Galleries of bark beetle larvae (Ips typographus) under the bark of a spruce tree in the French Alps. Close-up Photographer of the Year (CUPOTY) - Intimate Landscape Winner - A Network of Life and Death

    The Aiguille de Tré-la-Tête (3920 m) in the Mont Blanc massif (seen from the Petit Saint Bernard road in Italy).

    RM2596318JPG

    The Aiguille de Tré-la-Tête (3920 m) in the Mont Blanc massif (seen from the Petit Saint Bernard road in Italy).

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The Aiguille de Tré-la-Tête (3920 m) in the Mont Blanc massif (seen from the Petit Saint Bernard road in Italy).

    Mont Pourri and larch forest in autumn, Le Monal, Haute Tarentaise, Alps, France

    RM2596317JPG

    Mont Pourri and larch forest in autumn, Le Monal, Haute Tarentaise, Alps, France

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Mont Pourri and larch forest in autumn, Le Monal, Haute Tarentaise, Alps, France

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