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N2 and lava flows of the Grand Brulé on Reunion Island

Lanzarote Sea Rosemary or Balsam Spurge – Tetraena fontanesii (formerly known as Zygophyllum fontanesii) clings to life on a wind-scoured cliff in Lanzarote, its succulent leaves and tiny yellow flowers thriving where few plants dare. This Canary Islands endemic scoffs at drought, salt spray, and volcanic adversity. Its eaves store water and excrete salt through specialized glands

Ankarana Tsingy stones, northern Madagascar landmark

Volcanic features in the Craters of the Moon National Monument in Idaho. Both pahoehoe and aa lavas present in the park. Basaltic lava. Holocene-aged basaltic lava field. The Snake River Plain is a volcanic province that was created by a series of cataclysmic caldera-forming eruptions which started about 16 million years ago.

Fluid shapes in lava flow in Hawaii natural park - Big Island

Green shoots of plants growing up through black lava rock

erupting piton de la fournaise volcano panorama, africa, france, la reunion island.

Geldingardalir. aerial view of the Icelandic volcanic site. South Iceland, the site is very active and currently causing road disruptions throughout the geothermal area.

Volcanic rock piles on Big Island Hawaii

$Horta, Faial Island, Azores, Portugal: Faial Island, located in the central group of the Azores archipelago on the European tectonic plate near the Azores Triple Junction, is a volcanic landmass formed through submarine and subaerial eruptions spanning from over 800,000 years ago to the present. The island's geology comprises four main volcano-stratigraphic units, including the central Caldeira volcano—a truncated cone with a 2 km-wide summit crater reaching depths of 400 m and a maximum elevation of 1,043 m at Cabeço Gordo—and two principal fissure zones oriented WNW-ESE that intersect the central structure, facilitating overlapping eruptive episodes of nepheline- to hypersthene-normative basalts, hawaiites, and trachytes derived from partial melting of a heterogeneous, metasomatized garnet-bearing peridotite mantle source followed by fractional crystallization in crustal reservoirs. The western Capelo volcanic complex represents the youngest activity, exemplified by the 1957–1958 eruption at Capelinhos that added approximately 2.4 km² of new land through the formation of a cinder cone and isthmus, contributing to the island's irregular pentagonal shape, steep basaltic cliffs, lava arches, and diverse geomorphological features across its 173 km² area.$

Formica Leo crater at Piton de la Fournaise volcano, Reunion island, indian ocean, France

Green vegetation on volcanic rocks on Reunion Island

errupting piton de la fournaise volcano on la reunion island, french overseas territory, france.

A view from above of a manzanita growing on the side of Lava Butte in Newberry National Volcano Monument

It was recognized as a UNESCO Global Geopark by UNESCO in 13 and is the only geopark in Turkey. Aerial view of Kula Salihli UNESCO Global Geopark and Volcanic Park and Divlit Tepe Volcanics in Manisa. A geopark located in Kula and Salihli districts of Manisa province in western Turkey, also known as Kula Volcanic Geopark and Kula Geopark,

Vegetation on the volcanic rocks of a mountain range on the island of Madeira, Portugal

$Ferns and lichens in lava flow, Reunion Island, Piton de la Fournaise lava flow in the East. Tiny lava tube in the pahoehoe lavas. \n\nForêt domaniale du Grand Brûlé$

coastal road with lava in La Reunion, France

Two green leaves poke through black lava at Volcanoes National Park.

Native Hawaiian plants emerge defiantly from lava fields on the Big Island, symbolizing nature’s resilience after volcanic eruption.

Glowing Lava Flowing From Volcano in Hawaii

Volcanic Rock Basaltic Formation in Canary Islands

Piton de la Fournaise volcano, Reunion island, indian ocean, France

A sprawling landscape of vibrant green vegetation extends below a moody and turbulent sky, capturing nature's untamed beauty and atmospheric wonder in its raw form.

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