Paleoshoreline

Source: Wikipedia, the free encyclopedia.

A paleoshoreline (ancient

perched coastline
is an ancient (fossil) shoreline positioned above the present shoreline.

Tides cause the ocean to advance and recede in a very short time scale, in most places about twice per day. Weather conditions can also cause short-term variations. Coastlines can also move by coastal erosion without a change in sea level. However, "sea level" refers to the average level over a relatively long period (years). This average sea level can advance and recede over much longer periods (thousands or millions of years), causing paleoshorelines which may be difficult to identify.

Just off the coast of parts of North America, in the last 15,000 years sea level has varied from over 100 metres (330 ft) below, to as high as 10 metres (33 ft) above its present level. That entire time, humans have lived in North America.[2]

A lake may also have a paleoshoreline.[3][4]

Paleoshorelines have also been inferred on Mars;[5][6] see Burgsvik Beds and Martian dichotomy.

Image of the Bering land bridge being inundated with rising sea level across time
Paleoshorelines illustrated: Beringia sea levels (blues) and land elevations (browns) measured in metres from 21,000 years ago to present

Scientific importance

Paleoshorelines capture valuable records of

archaeological significance.[7]

Examples

See also

References

  1. ^ "paleo-". dictionary.com. Retrieved 2020-12-31.
  2. ^ a b "Paleoshoreline Research".
  3. . Retrieved 2021-01-01.
  4. . Retrieved 2021-01-01.
  5. .
  6. ^ Barrett, Katherine (June 7, 2017). "Paleoshorelines, Time capsules of the ocean's ancient shorelines". Oceanbites. Retrieved 2020-12-29.
  7. ^ "Doggerland - The Europe That Was". Retrieved 2020-12-31.
  8. ^ "Cascadia Subduction Zone". oregon.gov. Retrieved 2020-12-31.
  9. ^ Ryall, Julian (19 September 2007). "Japan's Ancient Underwater "Pyramid" Mystifies Scholars". nationalgeographic.com. Archived from the original on August 7, 2019. Retrieved 2020-12-31.

External links and references