Construct · 4 fields · 4 citations
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In geotechnics heave is the upward movement of the ground, most famously frost heave, in which water migrating to a freezing front forms growing ice lenses that lift the soil and anything founded on it. Taber's The mechanics of frost heaving showed that the lifting comes from water drawn to the freezing zone rather than from the expansion of water already in the pores. The referent is a vertical ground movement measured as displacement, unrelated to a ship's rise and fall or the sideways offset of a fault.[1]
In structural geology heave is the horizontal component of the displacement across a dip-slip fault, paired with the throw, which is the vertical component, so that the two together resolve how far the rocks have moved past one another. Fossen's Structural geology defines heave and throw as the standard way to describe the separation seen on a fault in cross-section. The referent is a static horizontal offset measured on a fault, unrelated to a ship's motion or the lifting of frozen soil.[3]
In periglacial science, heave refers to frost heave, the rise of the ground surface as ice lenses grow in freezing soil. This meaning comes from Taber (1929) in The Journal of Geology.[4]
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