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  2. Cinder cone - Wikipedia

    en.wikipedia.org/wiki/Cinder_cone

    As the gas-charged lava is blown violently into the air, it breaks into small fragments that solidify and fall as either cinders, clinkers, or scoria around the vent to form a cone that often is symmetrical; with slopes between 30 and 40°; and a nearly circular ground plan. [4] Most cinder cones have a bowl-shaped crater at the summit. [2]

  3. Volcanic ash - Wikipedia

    en.wikipedia.org/wiki/Volcanic_ash

    The term volcanic ash is also often loosely used to refer to all explosive eruption products (correctly referred to as tephra), including particles larger than 2 mm. Volcanic ash is formed during explosive volcanic eruptions when dissolved gases in magma expand and escape violently into the atmosphere. The force of the gases shatters the magma ...

  4. Category:Explosive gases - Wikipedia

    en.wikipedia.org/wiki/Category:Explosive_gases

    Only pure chemicals belong here not fuel air mixtures to be here a gas must have an upper explosive limit of 100%. Pages in category "Explosive gases" The following 9 pages are in this category, out of 9 total.

  5. Explosive eruption - Wikipedia

    en.wikipedia.org/wiki/Explosive_eruption

    In volcanology, an explosive eruption is a volcanic eruption of the most violent type. A notable example is the 1980 eruption of Mount St. Helens. Such eruptions result when sufficient gas has dissolved under pressure within a viscous magma such that expelled lava violently froths into volcanic ash when

  6. Soil gas - Wikipedia

    en.wikipedia.org/wiki/Soil_gas

    The composition of gases present in the soil's pores, referred to commonly as the soil atmosphere or atmosphere of the soil, is similar to that of the Earth's atmosphere. [5] Unlike the atmosphere, moreover, soil gas composition is less stagnant due to the various chemical and biological processes taking place in the soil. [5]

  7. Volcanic impacts on the oceans - Wikipedia

    en.wikipedia.org/wiki/Volcanic_impacts_on_the_oceans

    For example, the recovery time of ocean heat content of Pinatubo, which caused comparable radiative forcing to Krakatau, seems to be much shorter. This is because Pinatubo happened under a warm and non-stationary background with increasing greenhouse gas forcing. [7] However, its signal still could penetrate down to ~1000 m deep. [1]

  8. Limnic eruption - Wikipedia

    en.wikipedia.org/wiki/Limnic_eruption

    Lake Nyos, the site of a limnic eruption in 1986. A limnic eruption, also known as a lake overturn, is a very rare type of natural hazard in which dissolved carbon dioxide (CO 2) suddenly erupts from deep lake waters, forming a gas cloud capable of asphyxiating wildlife, livestock, and humans.

  9. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Water is the medium of the oceans, the medium which carries all the substances and elements involved in the marine biogeochemical cycles. Water as found in nature almost always includes dissolved substances, so water has been described as the "universal solvent" for its ability to dissolve so many substances.