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  2. Template:Supersonic shockwave cone.svg - Wikipedia

    en.wikipedia.org/wiki/Template:Supersonic...

    Main page; Contents; Current events; Random article; About Wikipedia; Contact us; Donate; Pages for logged out editors learn more

  3. Pyrometric cone - Wikipedia

    en.wikipedia.org/wiki/Pyrometric_cone

    The pyrometric cone is "A pyramid with a triangular base and of a defined shape and size; the "cone" is shaped from a carefully proportioned and uniformly mixed batch of ceramic materials so that when it is heated under stated conditions, it will bend due to softening, the tip of the cone becoming level with the base at a definitive temperature.

  4. Volcanic cone - Wikipedia

    en.wikipedia.org/wiki/Volcanic_cone

    A tuff cone, sometimes called an ash cone, is a small monogenetic volcanic cone produced by phreatic (hydrovolcanic) explosions directly associated with magma brought to the surface through a conduit from a deep-seated magma reservoir. They are characterized by high rims that have a maximum relief of 100–800 meters (330–2,620 ft) above the ...

  5. Ruspolia nitidula - Wikipedia

    en.wikipedia.org/wiki/Ruspolia_nitidula

    Ruspolia nitidula, the Large Conehead, is a species belonging to the subfamily Conocephalinae of the family Tettigoniidae. [1] It is found throughout Europe, Africa, and the Palearctic part of Asia. [2] A vernacular name that has been used is "cone-headed grasshopper", [3] although it is not a grasshopper, but rather a bush cricket. [4]

  6. Megafan - Wikipedia

    en.wikipedia.org/wiki/Megafan

    An alluvial megafan is a large cone or fan-shaped deposit built up by complex deposition patterns of stream flows originating from a single source point known as an apex. . Megafans differ from alluvial fans in their sheer si

  7. Malpaís de Güímar - Wikipedia

    en.wikipedia.org/wiki/Malpaís_de_Güímar

    Malpaís de Güímar or Badlands of Guimar consist of a volcanic cone, subsidiary cones, and several basaltic lava flows in the Güímar municipality on the island of Tenerife, in the Canary Islands, Spain. They total in area about 290 hectares. The lava flows are quite recent, with the typical ʻaʻā type less than 10,000 years old.

  8. Littoral cone - Wikipedia

    en.wikipedia.org/wiki/Littoral_cone

    The forming lava flows need to be sufficiently large; [14] the minimum size of lava flows that have formed such cones in Hawaiʻi is 38,000,000 cubic metres (50,000,000 cu yd). [15] Of these, about 5-6% of their volume is converted to fragments. [ 3 ]

  9. Hypercone - Wikipedia

    en.wikipedia.org/wiki/Hypercone

    In geometry, a hypercone (or spherical cone) is the figure in the 4-dimensional Euclidean space represented by the equation x 2 + y 2 + z 2 − w 2 = 0. {\displaystyle x^{2}+y^{2}+z^{2}-w^{2}=0.} It is a quadric surface, and is one of the possible 3- manifolds which are 4-dimensional equivalents of the conical surface in 3 dimensions.