What is the name of the volcanic cone in the eastern rift zone of the Kīlauea volcano of the Hawaiian Islands located in the middle of the As-Safa region?
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Al-Safa (Syria) As-Safa (Arabic: الصفا‎ ‎ , "Aṣ-Ṣafā" ), also known as Tulul al-Safa (تلول الصفا , "Tulūl Eṣ-Ṣafā" ), Arabic for "Al-Safa hills", is a hilly region which lies in southern Syria, north-east of Jabal Al-Arab volcanic plateau. It consists of a basaltic lava field of volcanic origin, covering an area of 220 square kilometres, and contains at least 38 cinder cones. This volcanic field lies within the northern part of the massive alkaline Harrat Ash Shamah volcanic field that extends from southern Syria, through eastern Jordan to Saudi Arabia. The region is extremely scarce in water. A boiling lava lake was observed in the Es Safa volcanic area in the middle of the 19th century (see Erta Ale in Ethiopia and Puʻu ʻŌʻō in Hawaii for reference).
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Puʻu ʻŌʻō Puʻ u ʻ Ōʻ ō (often written Puu Oo, ] ) is a volcanic cone in the eastern rift zone of the Kīlauea volcano of the Hawaiian Islands. Puʻ u ʻ Ōʻ ō has been erupting continuously since January 3, 1983, making it the longest-lived rift-zone eruption of the last two centuries.
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Virunga Mountains The Virunga Mountains (also known as Mufumbiro) are a chain of volcanoes in East Africa, along the northern border of Rwanda, the Democratic Republic of the Congo (DRC), and Uganda. The mountain range is a branch of the Albertine Rift Mountains, which border the western branch of the East African Rift. They are located between Lake Edward and Lake Kivu. The name "Virunga" is an English version of the Kinyarwanda word "ibirunga", which means "volcanoes".
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Lascar (volcano) Lascar is a stratovolcano within the Central Volcanic Zone of the Andes, a volcanic arc that spans the countries of Peru, Bolivia, Argentina and Chile. It is the most active volcano of the region, with records of eruptions going back to 1848. It is constructed from two separate cones with six or five summit craters. The westernmost crater of the eastern cone is presently active. Volcanic activity is characterized by constant release of volcanic gas and occasional Vulcanian eruptions.
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Tanganasoga Tanganasoga is the main volcano of El Hierro's El Golfo area in the Canary Islands, consisting of a cinder cone. The volcano is part of a much larger shield volcano system.
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Mount Marsabit Marsabit is a 6300 km² basaltic shield volcano in Kenya, located 170 km east of the center of the East African Rift, in Marsabit County near the town of Marsabit. This was primarily built during the Miocene, but some lava flows and explosive maar-forming eruptions have occurred more recently. At least two of the maars host crater lakes.
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Dead Sea Transform The Dead Sea Transform (DST) fault system, also sometimes referred to as the Dead Sea Rift, is a series of faults that run from the Maras Triple Junction (a junction with the East Anatolian Fault in southeastern Turkey) to the northern end of the Red Sea Rift (just offshore of the southern tip of the Sinai Peninsula). The fault system forms the transform boundary between the African Plate to the west and the Arabian Plate to the east. It is a zone of left lateral displacement, signifying the relative motions of the two plates. Both plates are moving in a general north-northeast direction, but the Arabian Plate is moving faster, resulting in the observed left lateral motions along the fault of approximately 107 km. A component of extension is also present in the southern part of the transform, which has contributed to a series of depressions, or pull-apart basins, forming the Gulf of Aqaba, Dead Sea, Sea of Galilee and Hula basins.
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Islands Region The Islands Region is one of four regions of Papua New Guinea (PNG) comprising the Bismarck Archipelago and north-eastern Solomon Islands Archipelago, located north-east of the mainland on eastern New Guinea island.
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Hawaiian–Emperor seamount chain The Hawaiian–Emperor seamount chain is a mostly undersea mountain range in the Pacific Ocean that reaches above sea level in Hawaii. It is composed of the Hawaiian ridge, consisting of the islands of the Hawaiian chain northwest to Kure Atoll, and the Emperor Seamounts: together they form a vast underwater mountain region of islands and intervening seamounts, atolls, shallows, banks and reefs along a line trending southeast to northwest beneath the northern Pacific Ocean. The seamount chain, containing over 80 identified undersea volcanoes, stretches over 5800 km from the Aleutian Trench in the far northwest Pacific to the Loʻihi seamount, the youngest volcano in the chain, which lies about 35 km southeast of the Island of Hawaiʻi.
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Niuafo'ou Plate The Niuafo'ou Plate is a small tectonic plate located west of the islands of Tonga. This plate is sandwiched between the Pacific Plate to the north, the very unstable Tonga Plate to the east and the Australian Plate to the west. It is primarily surrounded by convergent boundaries. This plate is riddled with active faults thus making the area extremely earthquake prone.
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Kawai Point Kawai Point is a jutting headland on the south-east coast of the island of Kauai in the Hawaiian Islands.
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2009 Tonga undersea volcanic eruption The 2009 Tonga undersea volcanic eruption began on March 16, 2009, near the island of Hunga Tonga, approximately 11 km from the Tongan capital of Tongatapu. The volcano is in a highly active volcanic region that represents a portion of the Pacific Ring of Fire. It is estimated that there are up to 36 undersea volcanoes clustered together in the area.
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Mahuika crater Mahuika crater is a submarine feature that is hypothesized to be an extraterrestrial impact crater. It is about 20 ± 2 km (12.4 ± 1.2 mi) wide and over 153 m deep and lies on the New Zealand continental shelf at 48.3 South and 166.4 East. The Mahuika crater is named after the Māori god of fire. However, there is debate about its origins.
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Dravuni Dravuni (pronounced ] ) is a volcanic island in the Kadavu Group of islands in Fiji. Covering an area of 0.8 km² , it is located at 18.78° South and 178.53° East, and reaches a maximum altitude of 40 m .
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Fanuatapu Fanuatapu is an uninhabited island which consists of a volcanic tuff ring, situated off the eastern tip of Upolu, Samoa. It is the smallest and easternmost of the four Aleipata Islands, with an area of 15 hectares, and has an automated lighthouse.
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Gufa Volcano The Gufa Volcano is a volcanic field located in the Southern Red Sea Region of Eritrea near the border with Djibouti. The peak elevation is 600 m where lava flows are visible. The last eruption of the volcano was inferred to be during the Holocene era.
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Kavachi Kavachi is one of the most active submarine volcanoes in the south-west Pacific Ocean. Located south of Vangunu Island in the Solomon Islands, it is named after a sea god of the New Georgia Group islanders, and is also referred to locally as Rejo te Kavachi ("Kavachi's oven’). The volcano has become emergent and then been eroded back into the sea at least eight times since its first recorded eruption in 1939.
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Arabian Basin The Arabian Basin is an oceanic basin located in the
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Honolulu Volcanic Series The Honolulu volcanic series is a set of monogenetic volcanic events on the Hawaiian island of Oahu. The events, which have been dated to between 800,000 and 30,000 years before the present, created several notable island features, including Diamond Head, the Punchbowl Crater, Hanauma Bay, Mānana Island and the youngest, Koko Crater. Most people don't consider those craters as volcanoes. They are thought to be extinct vents of the Ko'olau Range.
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East Melanesian Islands The East Melanesian Islands, also known as the Solomons-Vanuatu-Bismarck moist forests, is a biogeographic region in the Melanesia region of Oceania.
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Volcan Rumoka Volcan Rumoka, also known as Rumoka and Le Rumoka, is a cinder cone volcano in the Virunga Mountains in Nord Kivu, Democratic Republic of the Congo (formerly known as Zaire). The volcano is a minor satellite cone on the flanks of the massive shield volcano of Nyamuragira. It is located about 16 km (10 mi) south of Nyamuragira's caldera.
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Ardoukoba Ardoukôba (Arabic: أردوكوبا‎ ‎ ) is a fissure vents volcano in Djibouti. Located on the coast 100 km from Djibouti City, its summit is situated at 298 m above sea level. It last erupted in November 1978 following an earthquake, having been dormant for 3,000 years. The volcano's rift is 17 km in width, and has a depth of 800 m .