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Granite arch of Port Blanc, emblem of the Côte Sauvage de Quiberon, Hercynian granite eroded by the sea, Brittany, FranceGranite arch of Port Blanc, emblem of the Côte Sauvage de Quiberon, Hercynian granite eroded by the sea, Brittany, FranceGranite arch of Port Blanc, emblem of the Côte Sauvage de Quiberon, Hercynian granite eroded by the sea, Brittany, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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Granite arch of Port Blanc, emblem of the Côte Sauvage de

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The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, FranceThe Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, FranceThe Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496045

The Gardon de Sainte Croix in the Cévennes, very ancient

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The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, FranceThe Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, FranceThe Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496044

The Gardon de Sainte Croix in the Cévennes, very ancient

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The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, FranceThe Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, FranceThe Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496043

The Gardon de Sainte Croix in the Cévennes, very ancient

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The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, FranceThe Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, FranceThe Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496042

The Gardon de Sainte Croix in the Cévennes, very ancient

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Thongweed (Himanthalia elongata) at low tide on the Côte Sauvage de Quiberon, Brittany, FranceThongweed (Himanthalia elongata) at low tide on the Côte Sauvage de Quiberon, Brittany, FranceThongweed (Himanthalia elongata) at low tide on the Côte Sauvage de Quiberon, Brittany, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2489739

Thongweed (Himanthalia elongata) at low tide on the Côte Sauvage

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Granite arch of Port Blanc, emblem of the Côte Sauvage de Quiberon, Hercynian granite eroded by the sea, Brittany, FranceGranite arch of Port Blanc, emblem of the Côte Sauvage de Quiberon, Hercynian granite eroded by the sea, Brittany, FranceGranite arch of Port Blanc, emblem of the Côte Sauvage de Quiberon, Hercynian granite eroded by the sea, Brittany, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2489738

Granite arch of Port Blanc, emblem of the Côte Sauvage de

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Granite arch of Port Blanc, emblem of the Côte Sauvage de Quiberon, Hercynian granite eroded by the sea, Brittany, FranceGranite arch of Port Blanc, emblem of the Côte Sauvage de Quiberon, Hercynian granite eroded by the sea, Brittany, FranceGranite arch of Port Blanc, emblem of the Côte Sauvage de Quiberon, Hercynian granite eroded by the sea, Brittany, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2489737

Granite arch of Port Blanc, emblem of the Côte Sauvage de

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Mussels on blocks of Hercynian granite eroded by the sea at low tide, Côte Sauvage de Quiberon, Brittany, FranceMussels on blocks of Hercynian granite eroded by the sea at low tide, Côte Sauvage de Quiberon, Brittany, FranceMussels on blocks of Hercynian granite eroded by the sea at low tide, Côte Sauvage de Quiberon, Brittany, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2489735

Mussels on blocks of Hercynian granite eroded by the sea at low

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Mussels on blocks of Hercynian granite eroded by the sea at low tide, Côte Sauvage de Quiberon, Brittany, FranceMussels on blocks of Hercynian granite eroded by the sea at low tide, Côte Sauvage de Quiberon, Brittany, FranceMussels on blocks of Hercynian granite eroded by the sea at low tide, Côte Sauvage de Quiberon, Brittany, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2489734

Mussels on blocks of Hercynian granite eroded by the sea at low

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Pink granite of Ploumanac'h at dusk. 293 Ma old granite rich in pink feldspars, Ploumanac'h lighthouse, Côtes d'Armor, Brittany, FrancePink granite of Ploumanac'h at dusk. 293 Ma old granite rich in pink feldspars, Ploumanac'h lighthouse, Côtes d'Armor, Brittany, FrancePink granite of Ploumanac'h at dusk. 293 Ma old granite rich in pink feldspars, Ploumanac'h lighthouse, Côtes d'Armor, Brittany, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2489722

Pink granite of Ploumanac'h at dusk. 293 Ma old granite rich in

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Pink granite of Ploumanac'h at dusk. 293 Ma old granite rich in pink feldspars, Ploumanac'h lighthouse, Côtes d'Armor, Brittany, FrancePink granite of Ploumanac'h at dusk. 293 Ma old granite rich in pink feldspars, Ploumanac'h lighthouse, Côtes d'Armor, Brittany, FrancePink granite of Ploumanac'h at dusk. 293 Ma old granite rich in pink feldspars, Ploumanac'h lighthouse, Côtes d'Armor, Brittany, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2489721

Pink granite of Ploumanac'h at dusk. 293 Ma old granite rich in

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Pink granite of Ploumanac'h at dusk. 293 Ma old granite rich in pink feldspars, Ploumanac'h lighthouse, Côtes d'Armor, Brittany, FrancePink granite of Ploumanac'h at dusk. 293 Ma old granite rich in pink feldspars, Ploumanac'h lighthouse, Côtes d'Armor, Brittany, FrancePink granite of Ploumanac'h at dusk. 293 Ma old granite rich in pink feldspars, Ploumanac'h lighthouse, Côtes d'Armor, Brittany, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2489720

Pink granite of Ploumanac'h at dusk. 293 Ma old granite rich in

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Galets énormes de granite sur l'île Grande au crépuscule. Granites longtemps exploités intensivement (carrière de Castel-Erek), Côtes d'Armor, Bretagne, FranceGalets énormes de granite sur l'île Grande au crépuscule. Granites longtemps exploités intensivement (carrière de Castel-Erek), Côtes d'Armor, Bretagne, FranceGalets énormes de granite sur l'île Grande au crépuscule. Granites longtemps exploités intensivement (carrière de Castel-Erek), Côtes d'Armor, Bretagne, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2489653

Galets énormes de granite sur l'île Grande au crépuscule. Gr

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Galets énormes de granite sur l'île Grande au crépuscule. Granites longtemps exploités intensivement (carrière de Castel-Erek), Côtes d'Armor, Bretagne, FranceGalets énormes de granite sur l'île Grande au crépuscule. Granites longtemps exploités intensivement (carrière de Castel-Erek), Côtes d'Armor, Bretagne, FranceGalets énormes de granite sur l'île Grande au crépuscule. Granites longtemps exploités intensivement (carrière de Castel-Erek), Côtes d'Armor, Bretagne, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2489652

Galets énormes de granite sur l'île Grande au crépuscule. Gr

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Rose quartzRose quartzRose quartz© Marie Aymerez / BiosphotoJPG - RM
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Rose quartz

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The famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, FranceThe famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, FranceThe famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2446333

The famous Rosans sandstone balls: spheres formed by

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The famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, FranceThe famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, FranceThe famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2446332

2446332

The famous Rosans sandstone balls: spheres formed by

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The famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, FranceThe famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, FranceThe famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2446331

2446331

The famous Rosans sandstone balls: spheres formed by

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Exceptional granite of Hercynian age, rich in enormous nodules of biotite, surrounding a quartz nucleus, nodular granite of Castanheira, Geopark of Arouca, Portugal. These nodules are symbol of fertility in the local tradition (Pedras Parideiras)Exceptional granite of Hercynian age, rich in enormous nodules of biotite, surrounding a quartz nucleus, nodular granite of Castanheira, Geopark of Arouca, Portugal. These nodules are symbol of fertility in the local tradition (Pedras Parideiras)Exceptional granite of Hercynian age, rich in enormous nodules of biotite, surrounding a quartz nucleus, nodular granite of Castanheira, Geopark of Arouca, Portugal. These nodules are symbol of fertility in the local tradition (Pedras Parideiras)© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2437634

Exceptional granite of Hercynian age, rich in enormous nodules of

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Observation system of the nodular granite of Castanheira, Geopark of Arouca, Portugal. Exceptional granite of Hercynian age, rich in enormous nodules of biotite, surrounding a quartz nucleus, These nodules are symbol of fertility in the local tradition, Pedras Parideiras.Observation system of the nodular granite of Castanheira, Geopark of Arouca, Portugal. Exceptional granite of Hercynian age, rich in enormous nodules of biotite, surrounding a quartz nucleus, These nodules are symbol of fertility in the local tradition, Pedras Parideiras.Observation system of the nodular granite of Castanheira, Geopark of Arouca, Portugal. Exceptional granite of Hercynian age, rich in enormous nodules of biotite, surrounding a quartz nucleus, These nodules are symbol of fertility in the local tradition, Pedras Parideiras.© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2437625

Observation system of the nodular granite of Castanheira, Geopark

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AZURITE-MALACHITE ROCK, Cut and polished slab, Stepnoye Mine, Altay Mountains, Siberia, Russia, occurs in copper-bearing rocks in central Siberia, consists of white quartz with veins of the copper minerals azurite (blue) and malachite (green)AZURITE-MALACHITE ROCK, Cut and polished slab, Stepnoye Mine, Altay Mountains, Siberia, Russia, occurs in copper-bearing rocks in central Siberia, consists of white quartz with veins of the copper minerals azurite (blue) and malachite (green)AZURITE-MALACHITE ROCK, Cut and polished slab, Stepnoye Mine, Altay Mountains, Siberia, Russia, occurs in copper-bearing rocks in central Siberia, consists of white quartz with veins of the copper minerals azurite (blue) and malachite (green)© John Cancalosi / BiosphotoJPG - RMSale prohibited in Spain and Portugal
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2434419

AZURITE-MALACHITE ROCK, Cut and polished slab, Stepnoye Mine,

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Quartz Gecko (Pachydactylus latirostris)Quartz Gecko (Pachydactylus latirostris)Quartz Gecko (Pachydactylus latirostris)© Matthijs Kuijpers / BiosphotoJPG - RMNon exclusive sale
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2410592

Quartz Gecko (Pachydactylus latirostris)

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Verbena 'quartz burgundy' in a greenhouse in the spring, Pas de Calais, FranceVerbena 'quartz burgundy' in a greenhouse in the spring, Pas de Calais, FranceVerbena 'quartz burgundy' in a greenhouse in the spring, Pas de Calais, France© Yann Avril / BiosphotoJPG - RM
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2130799

Verbena 'quartz burgundy' in a greenhouse in the spring, Pas de

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Verbena 'quartz burgundy' in a greenhouse in the spring, Pas de Calais, FranceVerbena 'quartz burgundy' in a greenhouse in the spring, Pas de Calais, FranceVerbena 'quartz burgundy' in a greenhouse in the spring, Pas de Calais, France© Yann Avril / BiosphotoJPG - RM
2130798

2130798

Verbena 'quartz burgundy' in a greenhouse in the spring, Pas de

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spherulitic or orbicular chalcedony, "ocean jasper", Madagascar, cryptocrystaline quartzspherulitic or orbicular chalcedony, "ocean jasper", Madagascar, cryptocrystaline quartzspherulitic or orbicular chalcedony, "ocean jasper", Madagascar, cryptocrystaline quartz© John Cancalosi / BiosphotoJPG - RMSale prohibited in Spain and Portugal
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2078618

spherulitic or orbicular chalcedony, "ocean jasper", Madagascar,

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Hertfordshire puddingstone, Conglomerate sedimentary rock consisiting of flint pebbles cemented by quartz matrix, Hertfordshire EnglandHertfordshire puddingstone, Conglomerate sedimentary rock consisiting of flint pebbles cemented by quartz matrix, Hertfordshire EnglandHertfordshire puddingstone, Conglomerate sedimentary rock consisiting of flint pebbles cemented by quartz matrix, Hertfordshire England© John Cancalosi / BiosphotoJPG - RMSale prohibited in Spain and Portugal
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2077619

2077619

Hertfordshire puddingstone, Conglomerate sedimentary rock

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"Zebra stone", sedimentary rock from the east Kimberley of Western AustraliaComposed essentially of small particles of quartz and ‘sericite’ (fine-grained white mica), zebra rock also contains the minerals kaolinite, dickite and alunite. Known localities of the zebra rock lie close to the Ord River where the rock forms lenses and seams within the Johnny Cake Shale Member of the Ranford Formation, which formed during the late Precambrian (around 670 million years ago).
 Some seams of zebra rock are continuous over many kilometres.The colour banding of zebra rock probably formed by the rhythmic precipitation of iron oxide (hematite) rich bands during the alteration of the rock by percolating fluids (fluids migrating through the rock)."Zebra stone", sedimentary rock from the east Kimberley of Western AustraliaComposed essentially of small particles of quartz and ‘sericite’ (fine-grained white mica), zebra rock also contains the minerals kaolinite, dickite and alunite. Known localities of the zebra rock lie close to the Ord River where the rock forms lenses and seams within the Johnny Cake Shale Member of the Ranford Formation, which formed during the late Precambrian (around 670 million years ago).
 Some seams of zebra rock are continuous over many kilometres.The colour banding of zebra rock probably formed by the rhythmic precipitation of iron oxide (hematite) rich bands during the alteration of the rock by percolating fluids (fluids migrating through the rock)."Zebra stone", sedimentary rock from the east Kimberley of Western AustraliaComposed essentially of small particles of quartz and ‘sericite’ (fine-grained white mica), zebra rock also contains the minerals kaolinite, dickite and alunite. Known localities of the zebra rock lie close to the Ord River where the rock forms lenses and seams within the Johnny Cake Shale Member of the Ranford Formation, which formed during the late Precambrian (around 670 million years ago).
 Some seams of zebra rock are continuous over many kilometres.The colour banding of zebra rock probably formed by the rhythmic precipitation of iron oxide (hematite) rich bands during the alteration of the rock by percolating fluids (fluids migrating through the rock).© John Cancalosi / BiosphotoJPG - RMSale prohibited in Spain and Portugal
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2077618

2077618

"Zebra stone", sedimentary rock from the east Kimberley of

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Hertfordshire puddingstone, Conglomerate sedimentary rock consisiting of flint pebbles cemented by quartz matrix, Hertfordshire EnglandHertfordshire puddingstone, Conglomerate sedimentary rock consisiting of flint pebbles cemented by quartz matrix, Hertfordshire EnglandHertfordshire puddingstone, Conglomerate sedimentary rock consisiting of flint pebbles cemented by quartz matrix, Hertfordshire England© John Cancalosi / BiosphotoJPG - RMSale prohibited in Spain and Portugal
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2077615

2077615

Hertfordshire puddingstone, Conglomerate sedimentary rock

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Hertfordshire puddingstone ,conglomerate sedimentary rock composed of rounded flint pebbles cemented together by a younger matrix of silica quartz. The distinctive rock is largely confined to the English county of Hertfordshire but small amounts occur throughout the London BasinHertfordshire puddingstone ,conglomerate sedimentary rock composed of rounded flint pebbles cemented together by a younger matrix of silica quartz. The distinctive rock is largely confined to the English county of Hertfordshire but small amounts occur throughout the London BasinHertfordshire puddingstone ,conglomerate sedimentary rock composed of rounded flint pebbles cemented together by a younger matrix of silica quartz. The distinctive rock is largely confined to the English county of Hertfordshire but small amounts occur throughout the London Basin© John Cancalosi / BiosphotoJPG - RMSale prohibited in Spain and Portugal
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2077603

2077603

Hertfordshire puddingstone ,conglomerate sedimentary rock

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Orbicular jasper, "ocean jasper", Madagascar, a variety of jasper which contains variably-colored orbs or spherical inclusions or zones. In highly silicified rhyolite or tuff, quartz and feldspar crystallize in radial aggregates of needle-like crystals which provide the basis or seed for the orbicular structure seen in this kind of jasper.Orbicular jasper, "ocean jasper", Madagascar, a variety of jasper which contains variably-colored orbs or spherical inclusions or zones. In highly silicified rhyolite or tuff, quartz and feldspar crystallize in radial aggregates of needle-like crystals which provide the basis or seed for the orbicular structure seen in this kind of jasper.Orbicular jasper, "ocean jasper", Madagascar, a variety of jasper which contains variably-colored orbs or spherical inclusions or zones. In highly silicified rhyolite or tuff, quartz and feldspar crystallize in radial aggregates of needle-like crystals which provide the basis or seed for the orbicular structure seen in this kind of jasper.© John Cancalosi / BiosphotoJPG - RMSale prohibited in Spain and Portugal
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2077591

2077591

Orbicular jasper, "ocean jasper", Madagascar, a variety of jasper

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Cap d'Agde, rocks of yellow tuffs in regular layers, quartz, clay ... and basaltic rocks, Hérault, FranceCap d'Agde, rocks of yellow tuffs in regular layers, quartz, clay ... and basaltic rocks, Hérault, FranceCap d'Agde, rocks of yellow tuffs in regular layers, quartz, clay ... and basaltic rocks, Hérault, France© Thierry Le Quay / BiosphotoJPG - RM
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2074369

Cap d'Agde, rocks of yellow tuffs in regular layers, quartz, clay

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Leopard skin jasper, cryptocrystaline quartz, MexicoLeopard skin jasper, cryptocrystaline quartz, MexicoLeopard skin jasper, cryptocrystaline quartz, Mexico© John Cancalosi / BiosphotoJPG - RMSale prohibited in Spain and Portugal
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2070980

Leopard skin jasper, cryptocrystaline quartz, Mexico

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Sandstone balls the Serre Autruy - Baronnies Alpes France  ; Region of Saint André de Rosans: spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - their size can reach over a meter in diameter Sandstone balls the Serre Autruy - Baronnies Alpes France Sandstone balls the Serre Autruy - Baronnies Alpes France ; Region of Saint André de Rosans: spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - their size can reach over a meter in diameter © Jean-Philippe Delobelle / BiosphotoJPG - RM
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2036320

Sandstone balls the Serre Autruy - Baronnies Alpes France ;

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Sandstone balls the Serre Autruy - Baronnies Alpes France  ; Region of Saint André de Rosans: spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - their size can reach over a meter in diameter Sandstone balls the Serre Autruy - Baronnies Alpes France Sandstone balls the Serre Autruy - Baronnies Alpes France ; Region of Saint André de Rosans: spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - their size can reach over a meter in diameter © Jean-Philippe Delobelle / BiosphotoJPG - RM
2036319

2036319

Sandstone balls the Serre Autruy - Baronnies Alpes France ;

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Sandstone balls the Serre Autruy - Baronnies Alpes France  ; Region of Saint André de Rosans: spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - their size can reach over a meter in diameter Sandstone balls the Serre Autruy - Baronnies Alpes France Sandstone balls the Serre Autruy - Baronnies Alpes France ; Region of Saint André de Rosans: spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - their size can reach over a meter in diameter © Jean-Philippe Delobelle / BiosphotoJPG - RM
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2036318

Sandstone balls the Serre Autruy - Baronnies Alpes France ;

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Lichens on milky quartz block - Biella Alps Italy  ; Mount MucroneLichens on milky quartz block - Biella Alps Italy Lichens on milky quartz block - Biella Alps Italy ; Mount Mucrone© Jean-Claude Malausa / BiosphotoJPG - RM
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2017691

Lichens on milky quartz block - Biella Alps Italy ; Mount Mucrone

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Sandstone balls of Serre d'Autruy - Baronies France ; spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - reaching heights of over one meter in diameterSandstone balls of Serre d'Autruy - Baronies FranceSandstone balls of Serre d'Autruy - Baronies France ; spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - reaching heights of over one meter in diameter© Jean-Philippe Delobelle / BiosphotoJPG - RM
2011106

2011106

Sandstone balls of Serre d'Autruy - Baronies France ; spheres

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Sandstone balls of Serre d'Autruy - Baronies France ; spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - reaching heights of over one meter in diameterSandstone balls of Serre d'Autruy - Baronies FranceSandstone balls of Serre d'Autruy - Baronies France ; spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - reaching heights of over one meter in diameter© Jean-Philippe Delobelle / BiosphotoJPG - RM
2011105

2011105

Sandstone balls of Serre d'Autruy - Baronies France ; spheres

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Sandstone balls of Serre d'Autruy - Baronies France ; spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - reaching heights of over one meter in diameterSandstone balls of Serre d'Autruy - Baronies FranceSandstone balls of Serre d'Autruy - Baronies France ; spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - reaching heights of over one meter in diameter© Jean-Philippe Delobelle / BiosphotoJPG - RM
2011104

2011104

Sandstone balls of Serre d'Autruy - Baronies France ; spheres

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Sandstone balls of Serre d'Autruy - Baronies France ; spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - reaching heights of over one meter in diameterSandstone balls of Serre d'Autruy - Baronies FranceSandstone balls of Serre d'Autruy - Baronies France ; spheres formed by crystallization of quartz in the secondary age sandstones (- 110 ma) - reaching heights of over one meter in diameter© Jean-Philippe Delobelle / BiosphotoJPG - RM
2011103

2011103

Sandstone balls of Serre d'Autruy - Baronies France ; spheres

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Biggest quartz crystal in the world at Swakopmund in Namibia ; KRISTALL GALERIEBiggest quartz crystal in the world at Swakopmund in NamibiaBiggest quartz crystal in the world at Swakopmund in Namibia ; KRISTALL GALERIE© Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France
1906919

1906919

Biggest quartz crystal in the world at Swakopmund in Namibia ;

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Quartz crystal at Swakopmund in Namibia ; KRISTALL GALERIEQuartz crystal at Swakopmund in NamibiaQuartz crystal at Swakopmund in Namibia ; KRISTALL GALERIE© Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France
1906901

1906901

Quartz crystal at Swakopmund in Namibia ; KRISTALL GALERIE

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Quartz crystal at Swakopmund in Namibia ; KRISTALL GALERIEQuartz crystal at Swakopmund in NamibiaQuartz crystal at Swakopmund in Namibia ; KRISTALL GALERIE© Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France
1906897

1906897

Quartz crystal at Swakopmund in Namibia ; KRISTALL GALERIE

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Link of Blackstone Tombstone Territorial Park Yukon Canada ; North of Tombstone Territorial Park: quartzite mountains on the border of the Arctic, along the Dempster HighwayLink of Blackstone Tombstone Territorial Park Yukon CanadaLink of Blackstone Tombstone Territorial Park Yukon Canada ; North of Tombstone Territorial Park: quartzite mountains on the border of the Arctic, along the Dempster Highway© Jean-Philippe Delobelle / BiosphotoJPG - RM
1844384

1844384

Link of Blackstone Tombstone Territorial Park Yukon Canada ;

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Link of Blackstone Tombstone Territorial Park Yukon Canada ; North of Tombstone Territorial Park: quartzite mountains on the border of the Arctic, along the Dempster HighwayLink of Blackstone Tombstone Territorial Park Yukon CanadaLink of Blackstone Tombstone Territorial Park Yukon Canada ; North of Tombstone Territorial Park: quartzite mountains on the border of the Arctic, along the Dempster Highway© Jean-Philippe Delobelle / BiosphotoJPG - RM
1844383

1844383

Link of Blackstone Tombstone Territorial Park Yukon Canada ;

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Link of Blackstone Tombstone Territorial Park Yukon Canada ; North of Tombstone Territorial Park: quartzite mountains on the border of the Arctic, along the Dempster HighwayLink of Blackstone Tombstone Territorial Park Yukon CanadaLink of Blackstone Tombstone Territorial Park Yukon Canada ; North of Tombstone Territorial Park: quartzite mountains on the border of the Arctic, along the Dempster Highway© Jean-Philippe Delobelle / BiosphotoJPG - RM
1844382

1844382

Link of Blackstone Tombstone Territorial Park Yukon Canada ;

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Link of Blackstone Tombstone Territorial Park Yukon Canada ; North of Tombstone Territorial Park: quartzite mountains on the border of the Arctic, along the Dempster HighwayLink of Blackstone Tombstone Territorial Park Yukon CanadaLink of Blackstone Tombstone Territorial Park Yukon Canada ; North of Tombstone Territorial Park: quartzite mountains on the border of the Arctic, along the Dempster Highway© Jean-Philippe Delobelle / BiosphotoJPG - RM
1844381

1844381

Link of Blackstone Tombstone Territorial Park Yukon Canada ;

RMRight Managed

JPG

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Link of Blackstone Tombstone Territorial Park Yukon Canada ; North of Tombstone Territorial Park: quartzite mountains on the border of the Arctic, along the Dempster HighwayLink of Blackstone Tombstone Territorial Park Yukon CanadaLink of Blackstone Tombstone Territorial Park Yukon Canada ; North of Tombstone Territorial Park: quartzite mountains on the border of the Arctic, along the Dempster Highway© Jean-Philippe Delobelle / BiosphotoJPG - RM
1844380

1844380

Link of Blackstone Tombstone Territorial Park Yukon Canada ;

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Metamorphic slate rock eroded by the sea and stones NorwayMetamorphic slate rock eroded by the sea and stones NorwayMetamorphic slate rock eroded by the sea and stones Norway© Roger Eritja / BiosphotoJPG - RMNon exclusive sale
1819030

1819030

Metamorphic slate rock eroded by the sea and stones Norway

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