Lava tubeW
Lava tube

A lava tube, or pyroduct, is a natural conduit formed by flowing lava from a volcanic vent that moves beneath the hardened surface of a lava flow. If lava in the tube empties, it will leave a cave.

Algar do CarvãoW
Algar do Carvão

The Algar do Carvão is an ancient lava tube or volcanic vent located in the central part of the island of Terceira in the Portuguese archipelago of the Azores. It lies within the civil parish of Porto Judeu in the municipality of Angra do Heroísmo.

Arnold Lava Tube SystemW
Arnold Lava Tube System

The Arnold Lava Tube System is series of lava tubes in Deschutes County, Oregon, in the United States. It is located several miles southeast of the city of Bend. The system starts in the Deschutes National Forest on the northern flank of Newberry Volcano, heads northeast onto BLM land before finally terminating on private property near Horse Ridge. The system acted as a conduit for the lavas from Lava Top Butte that later fed the Badlands rootless shield. The lava flow that created the Arnold system is also referred to as the basalt of Lava Top Butte and is related to the Horse Cave lobe which is a lava flow that created the Horse Lava Tube System. The lava flows of Lava Top Butte, the Badlands, the Horse system, and the Arnold system all have a geologic age around 80,000 years old.

Cheese CaveW
Cheese Cave

Cheese Cave is a lava tube located in Gifford Pinchot National Forest just southwest of Trout Lake, Washington. It is approximately 2,060 feet (628 m) in length, with a mostly flat floor 25 feet (8 m) wide and a 45 feet (14 m) to 60 feet (18 m) high ceiling.

Craters of the Moon National Monument and PreserveW
Craters of the Moon National Monument and Preserve

Craters of the Moon National Monument and Preserve is a U.S. national monument and national preserve in the Snake River Plain in central Idaho. It is along US 20, between the small towns of Arco and Carey, at an average elevation of 5,900 feet (1,800 m) above sea level. The protected area's features are volcanic and represent one of the best-preserved flood basalt areas in the continental United States.

Cueva del VientoW
Cueva del Viento

Cueva del Viento is the largest lava tube system in Europe, and the fifth largest in the world, behind a series of lava tubes in Hawaii. It is also considered the most complex volcanic tube in the world, due to its morphology of several levels and passages.

Derrick CaveW
Derrick Cave

Derrick Cave is a lava tube located in the remote northwest corner of Lake County, Oregon. The cave is approximately 1,200 feet (370 m) long. It is up to 80 feet (24 m) wide and 46 feet (14 m) high in places. It was named in honor of H.E. Derrick, a pioneer rancher with a homestead 3 miles (4.8 km) southeast of the cave. The land around the cave is managed by the United States Department of Interior, Bureau of Land Management. Derrick Cave is open to the public year-round; however, camping is no longer permitted in the cave.

El Malpais National MonumentW
El Malpais National Monument

El Malpais National Monument is a National Monument located in western New Mexico, in the Southwestern United States. The name El Malpais is from the Spanish term Malpaís, meaning badlands, due to the extremely barren and dramatic volcanic field that covers much of the park's area.

Fugaku Wind CaveW
Fugaku Wind Cave

Fugaku Wind Cave is a lava tube at the northern foot of Mount Fuji, Japan. It is the largest of the several lava tubes that are found in the Aokigahara forest in Fujikawaguchiko Town, Yamanashi Prefecture.

Furnas do CavalumW
Furnas do Cavalum

The Furnas do Cavalum are a group of four caves located in Machico, Madeira. Named after a local legend about a demon called Cavalum, who was imprisoned in the cave.

Galerias da FeteiraW
Galerias da Feteira

The Galerias da Feteira is a geological feature in the civil parish of Feteira in the municipality of Angra do Heroísmo, on the Portuguese island of Terceira Island in the archipelago of the Azores.

Grotta del GeloW
Grotta del Gelo

Grotta del Gelo is a volcanic cave of Mount Etna which is known for the presence of a large amount of ice. The cave formed in 1614-1624 during a large eruption of the volcano, inside one of the lava flows produced during that eruption. Within the two subsequent decades, ice grew and accumulated in the cave. Today it is a tourist destination.

Gruta Brisa AzulW
Gruta Brisa Azul

The Gruta Brisa Azul, sometimes Gruta Bela Azul, is a geological feature situated in the civil parish of Feteira, in the municipality of Angra do Heroísmo, in the Portuguese archipelago of the Azores.

Gruta das Cinco RibeirasW
Gruta das Cinco Ribeiras

The Gruta das Cinco Ribeiras is a cave situated in the southwest coast of Terceira, located in the civil parish of Cinco Ribeiras, municipality of Angra do Heroísmo, in the Portuguese archipelago of the Azores.

Gruta das TorresW
Gruta das Torres

Gruta das Torres, is a lava cave, a geological formation of volcanic origin formed from the flow and cooling of subterranean magma rivers. This formation is located outside the parish of Criação Velha, in the municipality of Madalena, on the western flanks of the island of Pico. The cave system formed from a series of pāhoehoe lava flows which originating from the Cabeço Bravo parasitic cone about 500 to 1500 years ago. The caves are a group of interconnected lava tubes between 0.5–22 metres (2–72 ft) width, created from both pāhoehoe and ʻaʻā types of lavas generated during different geological periods. It has a height between 1.1 and 15 metres (3.6–49 ft) and is located at an elevation of 300 metres (980 ft). With an estimated length of over 5.2 km (3.2 mi) it is the longest lava cave in the Azores. Access to the cave was managed by the Mountaineering Association. Starting in 2011, AZORINA, SA took over the management and organization of the cave.

Gruta do CarvãoW
Gruta do Carvão

The Gruta do Carvão is an ancient lava tube located on the outskirts of the municipality of Ponta Delgada on the island of São Miguel in the Portuguese archipelago of the Azores.

Gruta do NatalW
Gruta do Natal

Gruta do Natal, also known as Galeria Negra or Gruta do Cavalo, is a cave system in municipality of Praia da Vitória, on the island of Terceira in the Portuguese archipelago of the Azores.

Hālona BlowholeW
Hālona Blowhole

Hālona Blowhole is a rock formation and a blowhole on the island of Oahu, Hawaii off of Hanauma Bay at Hālona Point overlooking the Pacific Ocean. In Hawaiian hālona means "lookout".

Horse Lava Tube SystemW
Horse Lava Tube System

The Horse Lava Tube System is a series of lava tubes within Deschutes County, Oregon, of the United States. The system starts within the Deschutes National Forest on the northern flank of Newberry Volcano and heads north into and near the city of Bend. The system continues north again to Redmond at the Redmond Caves and into the Redmond Canyon, where the last known segment is known to exist; however, the basalt flow that created the system goes beyond to Crooked River Ranch and terminates just short of the Crooked River Gorge. The lava flow that created the Horse system is also referred to as the Horse Cave lobe and it filled the ancient channel of the Deschutes River which at that time flowed around the east side of Pilot Butte. The Horse Cave lobe is a part of the basalt of Lava Top Butte which also consists of the Arnold Lava Tube System, the Badlands rootless shield, and the Lava Top butte basalt. All have a geologic age around 80,000 years old.

Jameos del AguaW
Jameos del Agua

Jameos del Agua is a series of lava caves, located in the municipality of Haría in northern Lanzarote, Canary Islands, Spain. It is also an art, culture and tourism center, created by local artist and architect, César Manrique, and managed by the government of Lanzarote. Jameos del Agua consists of a subterranean salt lake, restaurant, gardens, emerald-green pool, museum and auditorium.

Jeju Volcanic Island and Lava TubesW
Jeju Volcanic Island and Lava Tubes

The Jeju Volcanic Island and Lava Tubes is a World Heritage Site in South Korea.

Kazumura CaveW
Kazumura Cave

Kazumura Cave is a lava tube and has been surveyed at 40.7 miles long and 3,614 feet deep making it the longest and deepest lava tube in the world. The cave is located on the island of Hawaiʻi on the eastern slope of Kīlauea. Kīlauea is the most recently active volcano on the Big Island. The ʻAilāʻau lava flow that contains Kazumura Cave originated from the Kīlauea Iki Crater about 500 years ago.

Kuna CavesW
Kuna Caves

Kuna Caves are lava tubes found south of Kuna, Idaho. There is currently one publicly known entrance to the cave, an opening in the ground with a caged ladder leading down into the cave.

Lake Sai Bat CaveW
Lake Sai Bat Cave

Lake Sai Bat Cave is the largest of the several lava tubes that are near Lake Sai, in the Aokigahara forest in the northern side of Mount Fuji, Japan. It is known as a cave where visitors can observe the bats which live there.

Lava Beds National MonumentW
Lava Beds National Monument

Lava Beds National Monument is located in northeastern California, in Siskiyou and Modoc counties. The monument lies on the northeastern flank of Medicine Lake Volcano and has the largest total area covered by a volcano in the Cascade Range.

Lava River CaveW
Lava River Cave

The Lava River Cave near Bend, Oregon, is part of the Newberry National Volcanic Monument, which is managed by the United States Forest Service. At 5,211 feet (1,588 m) in length, the northwest section of the cave is the longest continuous lava tube in Oregon. While the cave's discovery in 1889 was officially credited to a pioneer hunter, the presence of obsidian flakes near the cave has led archaeologists to conclude that Native Americans knew about the cave long before settlers arrived in central Oregon.

Lava River Cave (Arizona)W
Lava River Cave (Arizona)

Lava River Cave is a lava tube in northern Arizona's Coconino National Forest. At approximately 0.75-mile (1.21 km) long, it is the longest cave of its kind known in Arizona. The cave was discovered by some lumbermen in 1915 and has historically been referred to as "Government Cave" due to its location on the eastern edge of Government Prairie and southeast of Government Peak. Today, Lava River Cave is freely accessible to the general public.

Lunar lava tubeW
Lunar lava tube

Lunar lava tubes are tunnels on the Moon that are thought to have formed during basaltic lava flows. When the surface of a lava tube cools, it forms a hardened lid that channels the lava as it continues to flow beneath the surface in a conduit-shaped passage. Once the flow of lava diminishes, the tunnel may drain, forming a hollow void. Lunar lava tubes are formed on sloped surfaces that range in angle from 0.4° to 6.5°. These tubes may be as wide as 500 metres (1,600 ft) before they become unstable against gravitational collapse. However, stable tubes may still be disrupted by seismic events or meteoroid bombardment.

Mammoth Cave (Utah)W
Mammoth Cave (Utah)

Mammoth Cave is a lava tube located on the Markagunt Plateau in the Dixie National Forest of Southern Utah, and is one of the largest lava tubes in Utah. The cave has over 2,200 feet of passage and is about a quarter mile long. It was formed by cooling lava and water less than 2,000 years ago. Due to moisture and its elevation of 8,050 feet above sea level the cave stays cool year round.

ManjanggulW
Manjanggul

The Manjanggul Lava Tube is located in Gimnyeong-ri, Gujwaeup, Jeju City. At up to 23m wide, 30m high and 8.928km long, it is the 12th-longest lava tube in the world and the second longest on Jeju island. It is regarded as having significant scientific and heritage value, owing to its excellent condition of preservation despite its age of formation.

Martian lava tubeW
Martian lava tube

Martian lava tubes are volcanic caverns on Mars that are believed to form as a result of fast-moving, basaltic lava flows associated with shield volcanism. Lava tubes usually form when the external surface of the lava channels cools more quickly and forms a hardened crust over subsurface lava flows. The flow eventually ceases and drains out of the tube, leaving a conduit-shaped void space which is usually several meters below the surface. Lava tubes are typically associated with extremely fluid pahoehoe lava. Gravity on mars is about 38% that of Earth's, allowing Martian lava tubes to be much larger in comparison.

Narusawa Ice CaveW
Narusawa Ice Cave

The Narusawa Ice Cave is a lava tube located in the Aokigahara forest, in the part that belongs to Narusawa Village, Yamanashi Prefecture, Japan. It is one of the three larger lava tubes at the northern foot of Mount Fuji, the other two caves being Fugaku Wind Cave and Lake Sai Bat Cave. All three were designated as Natural Monuments of Japan in 1929.

Newberry VolcanoW
Newberry Volcano

Newberry Volcano is a large active shield volcano located about 20 miles (32 km) south of Bend, Oregon, United States, 35 miles (56 km) east of the major crest of the Cascade Range, within the Newberry National Volcanic Monument. Its highest point is Paulina Peak. The largest volcano in the Cascade Volcanic Arc, Newberry has an area of 1,200 square miles (3,100 km2) when its lava flows are taken into account. From north to south, the volcano has a length of 75 miles (121 km), with a width of 27 miles (43 km) and a total volume of approximately 120 cubic miles (500 km3). It was named for the geologist and surgeon John Strong Newberry, who explored central Oregon for the Pacific Railroad Surveys in 1855. The surrounding area has been inhabited by Native American populations for more than 10,000 years.

Pluto's CaveW
Pluto's Cave

Pluto's Cave is a partially collapsed lava tube on the northern outskirts of Mount Shasta. Its main entrance is located close to the 99-97 Cutoff c. 12 miles (19 km) North-east of Weed and c. 14 miles (23 km) East-southeast of Grenada. The tube is roughly 190,000 years old, which is quite old for a lava tube, as they normally collapse quickly, having ceilings only a few metres thick. However, Pluto's Cave is located in a semi-arid climate, where erosion is restricted, which contributes to its survival.

RaufarhólshellirW
Raufarhólshellir

Raufarhólshellir is the fourth-longest lava tube in Iceland. The cave's proximity to Reykjavík made it popular with visitors, who caused damage to the cave. In late 2016 the cave was closed to the public to clear accumulated garbage and install lighting and a walkway to part of the cave. The cave reopened for guided tours the following year.

Redmond CavesW
Redmond Caves

The Redmond Caves are a group of six lava tubes in Deschutes County, Oregon, United States. The caves are located in the city of Redmond and are jointly managed by the city and the Bureau of Land Management (BLM). Five of the caves are in the Redmond Caves Park and have been known locally for many years. The caves are a part of the Horse Lava Tube System and are the farthest northern extent of the system. The lava flow that created both the Horse system and the Redmond Caves continued on into the Redmond Dry Canyon and terminated near Crooked River Ranch. The caves have a geologic age of about 80,000 years.

São Vicente CavesW
São Vicente Caves

The São Vicente Caves are caves located in the parish and county of São Vicente, Madeira. Entrance is charged at €8 for adults, but have been closed since March 2020.

Skeleton Cave (Oregon)W
Skeleton Cave (Oregon)

Skeleton Cave is a lava tube within Deschutes County, Oregon, of the United States. The cave is within Deschutes National Forest and is located on the northern flank of Newberry Volcano near the city of Bend. The cave is between 75,000 and 400,000 years old.

SurtshellirW
Surtshellir

Surtshellir is a lava cave located in western Iceland, around 60 km from the settlement of Borgarnes. Approximately a mile in length, it is the longest such cave in the country. It was the first known lava tube in the world, at least by modern speleologists, and remained the longest known lava tube until the end of the 19th century. While mentioned in the medieval historical-geographical work Landnámabók, Eggert Ólafsson was the first to give a thorough documentation of the cave in his 1750 travels of the region. It is named after the fire giant Surtr, a prominent figure in Norse mythology, who is prophesied to one day engulf the world in the fire of his flaming sword.

Cueva de los VerdesW
Cueva de los Verdes

Cueva de los Verdes is a lava tube and tourist attraction of the Haria municipality on the island of Lanzarote in the Canary Islands (Spain). The cave lies within the Monumento Natural del Malpaís de La Corona, a protected area of the Canary Islands.

VíðgelmirW
Víðgelmir

Víðgelmir is a lava tube situated in the Hallmundarhraun lava field in west Iceland, around 2 km southeast of Fljótstunga farm in Hvítársíða, Borgarfjörður. The roof of the lava tube has collapsed, creating two large openings near its north end which are the only known entrances. Víðgelmir is 1585 m long and the largest part of the cave passage is 15.8 m high and 16.5 m wide, making it by far the largest of its kind in Iceland. The cave has a wide entrance but narrows down in some places. An iron gate was installed at the first constriction in 1991 to preserve those of the delicate lava formations or speleothems which hadn't already been destroyed. Evidence of human habitation, probably dating to the Viking Age, has been discovered in the cave and is preserved in the National Museum of Iceland. Long stretches of the cave floor are very rough and shouldn't be navigated without a guide. Access and guided tours are provided at nearby Fljótstunga.

Wilson Butte CaveW
Wilson Butte Cave

Wilson Butte Cave is located on the Snake River plain in Jerome County northeast of Twin Falls and southeast of Shoshone, Idaho. Listed on the National Register of Historic Places as an archeological site, it is maintained by the Bureau of Land Management (BLM).

Wiri Lava CaveW
Wiri Lava Cave

Wiri lava cave is Auckland's longest known lava cave at around 290 metres. It is part of Matukutūruru volcano, in the Auckland volcanic field. Because it features rare lava stalactites the cave has garnered international renown. The cave entrance is locked and entry is by permit only.