Description
Circular to subcircular deposits of mud and rock breccia. These deposits range in diameter from few meters up to tens of kilometers. They can produce a variety of morphologies: domes, cones, caldera-like forms, or relatively flat structures, reflecting physical properties of the rising material (Oehler and Allen 2010). Their shape ranges from conical elevations to negative funnel-shaped forms (Dimitrov 2002).
Morphometry
On Earth, the size ranges typically from 10s of cm high and wide to over 1 km in diameter (Allen et al. 2009). On the deep seafloor they may be up to hundreds of m high and several km wide (van Loon 2010). In Azerbaijan, where they are found in the highest concentration on Earth with 20–40 mounds per 1,000 km2, their diameters are up to ~1–10 km, with heights of ~100–500 m (Amador et al. 2010).
Subtypes by Setting
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References
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Hargitai, H. (2014). Mud Volcano. In: Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-9213-9_510-1
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DOI: https://doi.org/10.1007/978-1-4614-9213-9_510-1
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