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  2. Eyjafjallajökull - Wikipedia

    en.wikipedia.org/wiki/Eyjafjallajökull

    The south face of the mountain was once part of Iceland's coastline, from which, over thousands of years, the sea has retreated some 5 km (3 mi). The former coastline now consists of sheer cliffs with many waterfalls, of which the best known is Skógafoss. In strong winds, the water of the smaller falls can even be blown up the mountain.

  3. Geology of South Georgia and the South Sandwich Islands

    en.wikipedia.org/wiki/Geology_of_South_Georgia...

    The island of South Georgia is unusual among oceanic islands for having pre-Cretaceous sedimentary rocks underlying much of the island and a significant portion of felsic igneous rocks. Two-thirds of the island consists of intensely folded flysch , capped with Aptian age fossils, tuff and greywacke in the Cumberland Bay Series.

  4. South Sandwich Islands - Wikipedia

    en.wikipedia.org/wiki/South_Sandwich_Islands

    The territory of "South Georgia and the South Sandwich Islands" was formed in 1985; [2] previously, both archipelagos had been governed as part of the Falkland Islands Dependencies. On 10 February 2008, an earthquake of magnitude 6.5 on the Richter Scale had its epicenter 205 km (127 mi) south-southeast of Bristol Island . [ 3 ]

  5. 2010 eruptions of Eyjafjallajökull - Wikipedia

    en.wikipedia.org/wiki/2010_eruptions_of...

    Eyjafjallajökull (pronounced [ˈeiːjaˌfjatlaˌjœːkʏtl̥] ⓘ) is one of Iceland's smaller ice caps located in the far south of the island. Situated to the north of Skógar and to the west of the larger ice cap Mýrdalsjökull , Eyjafjallajökull covers the caldera of a volcano 1,666 m (5,466 ft) high, which has erupted relatively ...

  6. List of volcanic eruptions in Iceland - Wikipedia

    en.wikipedia.org/wiki/List_of_volcanic_eruptions...

    [citation needed] The lava flowed south and formed the basin of Þingvallavatn, Iceland's largest lake. 8230 BC - Grímsvötn The eruption was VEI 6, producing some 15 km 3 (3.6 cu mi) of tephra, resulting in the Saksunarvatn tephra. [112] [113] (Part of the East volcanic zone (EVZ)) Circa 6,800 BC Theistareykjarbunga (Þeistareykjarbunga).

  7. Alpine orogeny - Wikipedia

    en.wikipedia.org/wiki/Alpine_orogeny

    The Alpine orogeny is caused by the continents Africa, Arabia and India and the small Cimmerian Plate colliding (from the south) with Eurasia in the north. Convergent movements between the tectonic plates (the African Plate, the Arabian Plate and the Indian Plate from the south, the Eurasian Plate and the Anatolian Sub-Plate from the north, and many smaller plates and microplates) had already ...

  8. In recent years, the construction of large-scale solar farms in South and Middle Georgia has become a key part of the state’s energy plans — and crucial if Georgia’s coal plants are to be ...

  9. Geology of Georgia (country) - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Georgia_(country)

    The geology of Georgia is the study of rocks, minerals, water, landforms and geologic history in Georgia. The country is dominated by the Caucasus Mountains at the junction of the Eurasian Plate and the Afro-Arabian Plate, and rock units from the Mesozoic and Cenozoic are particularly prevalent.