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Kipuka

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Encyclopedia of Planetary Landforms

Definition

An island of older rock embayed and surrounded by younger lava (Larson 1992).

Synonyms

Steptoe

Morphometry

There is no size limit determined for kipukas.

Formation

Formed by volcanic accumulation at and burial of the surroundings of a rock; in contrast to outliers (plateau) that form by erosion of the surroundings.

Significance

Distinguishing structures that predate a lava flow (i.e., kipukas) from those that are superposed on lava flows is important in determining stratigraphic relationships (and emplacement history) of units (e.g., volcanic cones on Venus: Ivanov and Head 2004, impact craters on Mercury: Murchie et al. 2008).

Planetary Analogues

Venus: small volcanoes that may be embayed by regional plains (Kreslavsky and Head 1999) or shield fields (Ivanov and Head 2004). Moon: Darney Chi (Cognitum Kipuka), Aristarchus Plateau (Nichols et al. 1974) kipukas of highland material adjacent to mare domes (Head and Gifford 1980; Fig. 1). Mars: the Columbia Hills represent a...

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References

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Correspondence to Henrik Hargitai .

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© 2014 Springer Science+Business Media New York

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Hargitai, H. (2014). Kipuka. In: Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-9213-9_205-1

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  • DOI: https://doi.org/10.1007/978-1-4614-9213-9_205-1

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  • Online ISBN: 978-1-4614-9213-9

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