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Green plants grow from black lava in Hawaii.
Fluid shapes in lava flow in Hawaii natural park - Big Island
Landscape scenery of Shetani lava flow tsavo west national park Kenya
Interesting patterns made by Cooled Solid Lava on Hawaii Big Island.
A scenic view of one of the many lava fields on Bartomome Island.  Bartolome is one of the youngest islands in the Galapagos and displays a fantastic landscape of lava formations.
Barren land in Volcanoes national park, lava field
Hardened lava against the mountains of the big island of Hawaii.
The edge of the lava field, tephra. Volcanic lava goes around the hill and the forest island: dwarf alder (Alnus kamtschatica), birch (Betulaceae) remains. Kamchatka
The hia lehua, Metrosideros polymorpha, is a species of flowering evergreen tree in the myrtle family, Myrtaceae, that is endemic to the six largest islands of Hawaii.  Many native Hawaiian traditions refer to the tree and the forests it forms as sacred to Pele, the volcano goddess, and to Laka, the goddess of hula. Hawaii Volcanoes National Park,  Hawaii, The Big Island. Pioneer species.
coastal lava field and vegetation abutting cliffs along ala kahakai national trail at alahaka bay in south kona hawaii
Volcanic Lava Falls in El Malpais National Monument in Grants, New Mexico Southwest United States
Afar Triangle or Danakil Depression
Ferns and lichens in lava flow, Reunion Island, Piton de  la Fournaise lava flow in the East. Tiny lava tube in the pahoehoe lavas. Rope lavas.\n\nForêt domaniale du Grand Brûlé
Baranco Esquinzo (Fuerteventura, Canary 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
The Tseax Lava bed is the result of a major lava flow eruption around 1750. The flow travelled north to the Nass River, where it filled the flat valley floor and destroyed a Nisga'a community.
Teide National Park, Tenerife - the most spectacular travel destination, lava and Canary Island pine tree
Black desert after volcano eruption, cooled lava field with cracks and few plants on the horizon. Big Island, Hawaii, the USA.
Vertical photograph of lava terrain and crevasses in the area near the Bridge Between Continents on the Reykjanes Peninsula during a cloudy day
It is a raw material that only a volcanic area like Catania with its immense Etna can use. The Etna lava stone has become a treasure and a great resource for the local economy.
Volcanic rock piles on Big Island Hawaii
Black basalt volcanic rock on the Big Island of Hawaii.
Desert land with black lava basalt formations, volcanic soil on which cacti and thorny bushes grow in a hot tropical climate.
The Tseax Lava bed is the result of a major lava flow eruption around 1760 that travelled into the Tseax River, damming it and forming Lava Lake. The flow subsequently travelled 11 km (7 mi) north to the Nass River, where it filled the flat valley floor for an additional 10 km (6 mi), making the entire lava flow approximately 22.5 km (14 mi) long
coastal road with  lava in La Reunion, France
Sparse vegetation around Montanña de Mazo o Negra on volcanic Canary island Lanzarote
Closeup of some interesting lava rock at Valley of Fires Recreation Area, New Mexico
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.
Volcanic Rock Basaltic Formation in Canary Islands
Scenery at Valley of Fire Recreation Area, New Mexico, USA
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