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History

Soil Types

  • Alfisols: Low to moderate elevations in humid subtropical, humid continental, and Mediterranean climates. They are likely to be deposited by rivers.

  • Andisols: Various elevations, often highlands, in marine west coast, humid subtropical, and tropical rainforest climates.

  • Aridisols: Various elevations, often lowland deserts, in hot and cold desert climates.

  • Entisols: Various elevations, from floodplains to mountains, in a wide range of climates. They are likely to be deposited by rivers.

  • Gelisols: Low to moderate elevations in tundra and ice cap climates.

  • Histosols: Lowland areas in wetlands within humid continental and marine west coast climates.

  • Inceptisols: Various elevations, from floodplains to mountains, in a wide range of climates. They are likely to be deposited by rivers.

  • Mollisols: Low to moderate elevations in cold semi-arid and humid continental climates. They are likely to be deposited by rivers.

  • Oxisols: Various elevations, often in tropical lowlands, in tropical rainforest and tropical savanna climates.

  • Spodosols: Low to moderate elevations in subarctic and humid continental climates.

  • Ultisols: Various elevations, often in hilly or upland areas, in humid subtropical and tropical rainforest climates.

  • Vertisols: Various elevations, often in flat or gently sloping areas, in semi-arid steppe and humid subtropical climates.

  • Shield Volcanoes: Broad, gentle slopes; formed by low-viscosity basaltic lava; non-explosive eruptions.

    • Common Locations: Hot spots (e.g., Hawaiian Islands), divergent plate boundaries (e.g., Iceland).
  • Stratovolcanoes: Steep, conical; formed by alternating layers of lava and volcanic debris; explosive eruptions.

    • Common Locations: Convergent plate boundaries (e.g., Pacific Ring of Fire), volcanic arcs.
  • Cinder Cone Volcanoes: Small, steep slopes; formed by volcanic debris; short-lived and moderately explosive.

    • Common Locations: Flanks of larger volcanoes, rift zones, volcanic fields.
  • Lava Domes: Steep-sided, dome-like; formed by highly viscous lava; potential for explosive activity.

    • Common Locations: Volcanic arcs, continental volcanic regions, associated with stratovolcanoes and caldera complexes.

Significance

See Also