When.com Web Search

Search results

  1. Results From The WOW.Com Content Network
  2. Cinder cone - Wikipedia

    en.wikipedia.org/wiki/Cinder_cone

    A cinder cone (or scoria cone [1]) is a steep conical hill of loose pyroclastic fragments, such as volcanic clinkers, volcanic ash, or scoria that has been built around a volcanic vent. [ 2 ] [ 3 ] The pyroclastic fragments are formed by explosive eruptions or lava fountains from a single, typically cylindrical, vent.

  3. Volcanic cone - Wikipedia

    en.wikipedia.org/wiki/Volcanic_cone

    Cinder cones typically only erupt once like Parícutin. As a result, they are considered to be monogenetic volcanoes and most of them form monogenetic volcanic fields. Cinder cones are typically active for very brief periods of time before becoming inactive. Their eruptions range in duration from a few days to a few years. Of observed cinder ...

  4. Volcanic field - Wikipedia

    en.wikipedia.org/wiki/Volcanic_field

    Scoria cones are particularly prone to cluster into volcanic fields, which are typically 30–80 kilometers (19–50 miles) in diameter and consist of several tens to several hundred individual cones. The unusually large Trans-Mexican Volcanic Belt has nearly 1000 cones covering an area of 60,000 square kilometers (23,000 sq mi). [5]

  5. List of cinder cones - Wikipedia

    en.wikipedia.org/wiki/List_of_cinder_cones

    Lava Butte, a cinder cone in Newberry National Volcanic Monument, Oregon. A list of cinder cones is shown below. This list is incomplete; ...

  6. Scoria - Wikipedia

    en.wikipedia.org/wiki/Scoria

    The geological term cinder is synonymous and interchangeable with scoria, though scoria is preferred in scientific literature. [ 2 ] [ 4 ] The word comes from Greek σκωρία, skōria , rust. In earlier terminology, scoria was usually defined with a size range, e.g. 2 to 24 mm (0.079 to 0.945 in) in diameter, but neither color nor ...

  7. Monogenetic volcanic field - Wikipedia

    en.wikipedia.org/wiki/Monogenetic_volcanic_field

    Many monogenetic volcanoes are cinder cones, often with lava flows, such as Parícutin in the Michoacán-Guanajuato volcanic field, which erupted from 1943 to 1952. Some monogenetic volcanoes are small lava shields, such as Rangitoto Island in the Auckland volcanic field.

  8. Strombolian eruption - Wikipedia

    en.wikipedia.org/wiki/Strombolian_eruption

    The tephra accumulates in the vicinity of the vent, forming a cinder cone. Cinder is the most common product; the amount of volcanic ash is typically rather minor. The lava flows are more viscous, and therefore shorter and thicker, than the corresponding Hawaiian eruptions; it may or may not be accompanied by production of pyroclastic rock.

  9. Pisgah Crater - Wikipedia

    en.wikipedia.org/wiki/Pisgah_Crater

    Pisgah Crater, or Pisgah Volcano, is a young volcanic cinder cone rising above a lava plain in the Mojave Desert, between Barstow and Needles, California in San Bernardino County, California. The volcanic peak is around 2.5 miles (4.0 km) south of historic U.S. Route 66 - National Old Trails Highway and of Interstate 40 , and west of the town ...