Stóra-Eldborg Undir Geitahlíð
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Stóra-Eldborg Undir Geitahlíð
Stóra-Eldborg undir Geitahlíð (; also Stóra-Eldborg við Geitahlíð ) is a small Holocene volcano in Iceland, on Reykjanes peninsula, 50 m high,Íslandshandbókin. Náttúra, saga of sérkenni. Reykjavík 1989, p. 45 with a 30 m deep crater.Reynir Ingibjartsson: 25 Gönguleiðir á Reykjanesskaga. Náttúrann við Bæjarveggin. Reykjavík , p.112 - 117 It is located at about 5 km from Krýsuvík and as the name says at the foot of a bigger mountain, the tuya of ''Geitahlíð''. Volcanism Eruption fissures of the Brennisteinsfjöll volcanic system Despite its location, just some 5 km from the high temperature area of Seltún, the volcano and its counterparts, the crater rows, fissures, as well as the tuya ''Geitahlíð'' (385 m) with the crater Æsubúðir on its top, are not part of the Krýsuvík volcanic system, but of the volcanic system of Brennisteinsfjöll as its southernmost outpost. Eldborgir erupted about 2400 BP. The crater row also includes some ...
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Pyroclastic Cone
Volcanic cones are among the simplest volcanic landforms. They are built by ejecta from a volcanic vent, piling up around the vent in the shape of a cone with a central crater. Volcanic cones are of different types, depending upon the nature and size of the fragments ejected during the eruption. Types of volcanic cones include stratocones, spatter cones, tuff cones, and cinder cones. Stratocone Stratocones are large cone-shaped volcanoes made up of lava flows, explosively erupted pyroclastic rocks, and igneous intrusives that are typically centered around a cylindrical vent. Unlike shield volcanoes, they are characterized by a steep profile and periodic, often alternating, explosive eruptions and effusive eruptions. Some have collapsed craters called calderas. The central core of a stratocone is commonly dominated by a central core of intrusive rocks that range from around to over several kilometers in diameter. This central core is surrounded by multiple generations of lava f ...
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