Geological event

Source: Wikipedia, the free encyclopedia.

A geological event is a temporary and spatially

stratigraphical record.[1]

Seismite in Holocene sediments of the Dead Sea basin, Israel. This is a record of an earthquake (a geological event) that disturbed the strata.

Geological events range in time span by orders of magnitude, from seconds to millions of years, and in spatial scale from local to regional and, ultimately, global.

isochronous
.

Examples of geological events include a single footprint, an

geologic time.[7][8]

References

  1. ^ Ager, D. V. (1973). The Nature of the Stratigraphic Record. Wiley.
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