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  2. 1815 eruption of Mount Tambora - Wikipedia

    en.wikipedia.org/wiki/1815_eruption_of_Mount_Tambora

    Mount Tambora experienced several centuries of dormancy before 1815, caused by the gradual cooling of hydrous magma in its closed magma chamber. [7] Inside the chamber at depths between 1.5 and 4.5 km (5,000 and 15,000 ft), the exsolution of a high-pressure fluid magma formed during cooling and crystallisation of the magma.

  3. Mount Tambora - Wikipedia

    en.wikipedia.org/wiki/Mount_Tambora

    Mount Tambora, or Tomboro, is an active stratovolcano in West Nusa Tenggara, Indonesia. Located on Sumbawa in the Lesser Sunda Islands, it was formed by the active subduction zones beneath it. Before the 1815 eruption, its elevation reached more than 4,300 metres (14,100 feet) high, making it one of the tallest peaks in the Indonesian archipelago.

  4. Year Without a Summer - Wikipedia

    en.wikipedia.org/wiki/Year_Without_a_Summer

    Paintings during the years before and after seem to confirm that these striking reds were not present before Mount Tambora's eruption, [41] [42] and depict moodier, darker scenes, even in the light of both the sun and the moon. Caspar David Friedrich's The Monk by the Sea (ca. 1808–1810) and Two Men by the Sea (1817) indicate this shift of ...

  5. File:Mount Tambora Volcano, Sumbawa Island, Indonesia.jpg

    en.wikipedia.org/wiki/File:Mount_Tambora_Volcano...

    The huge caldera—6 kilometers in diameter and 1,100 meters deep—formed when Tambora’s estimated 4,000-meter-high peak was removed, and the magma chamber below emptied during the 1815 eruption. Today the crater floor is occupied by an ephemeral freshwater lake, recent sedimentary deposits, and minor lava flows and domes emplaced during the ...

  6. List of Quaternary volcanic eruptions - Wikipedia

    en.wikipedia.org/wiki/List_of_Quaternary...

    Mount Tambora, Lesser Sunda Islands, Indonesia: 1815, Apr 10: 7: 160–213 km 3 (38–51 cu mi) of tephra: an estimated 10–120 million tons of sulfur dioxide were emitted, produced the "Year Without a Summer" [23] 1808 ice core event: Unknown eruption near equator, magnitude roughly half Tambora

  7. Tambora culture - Wikipedia

    en.wikipedia.org/wiki/Tambora_culture

    Tambora is a lost city and culture on Sumbawa Island buried by volcanic ash and pyroclastic flows from the massive 1815 eruption of Mount Tambora. The city had about 10,000 residents. Scientists unearthing the site have discovered ceramic pots, bronze bowls, glass bottles, and homes and inhabitants buried by ash in a manner similar to that of ...

  8. These stories, aided by photos or other artifacts, are so powerful partly because they are very real to us. #6 Lovely Remake Of Family Image credits: Vestiges of History

  9. Category:VEI-7 volcanoes - Wikipedia

    en.wikipedia.org/wiki/Category:VEI-7_volcanoes

    The only unambiguous VEI-7 eruption to have been directly observed in recorded history was Mount Tambora in 1815 and caused the Year Without a Summer in 1816. The Minoan eruption of Thera in the middle of the second millennium BC may have been VEI-7, but may have been just shy of the 100 cubic kilometers required.