Raised shoreline

In this article, we will explore the topic of Raised shoreline in depth. From its origin to its impact on today's society, we will analyze all the facets of Raised shoreline and its relevance in different contexts. Through a multidisciplinary approach, we will examine the various perspectives that exist regarding Raised shoreline, and explore how it has evolved over time. In addition, we will discuss its influence in areas such as culture, economics and politics, and reflect on its future in a constantly changing world. Get ready to embark on a journey of discovery about Raised shoreline and everything that this concept entails.

A raised shoreline is an ancient shoreline exposed above current water level.[1] These landforms are formed by a relative change in sea level due to global sea level rise, isostatic rebound, and/or tectonic uplift. These surfaces are usually exposed above modern sea level when a heavily glaciated area experiences a glacial retreat, causing water levels to rise. This area will then experience post-glacial rebound, effectively raising the shoreline surface.

Examples of raised shorelines can be found along the coasts of formerly glaciated areas in Ireland[2] and Scotland, as well as in North America. Raised shorelines are exposed at various locations around the Puget Sound of Washington State.[3]

See also

References

  1. ^ http://www.encyclopedia.com/doc/1O112-raisedshorelines.html [dead link‍]
  2. ^ http://www.askaboutireland.ie/.../changing-sea-levels/ [permanent dead link‍]
  3. ^ Kovanen, Dori J.; Slaymaker, Olav (December 2004). "Relict shorelines and ice flow patterns of the northern puget lowland from lidar data and digital terrain modelling". Geografiska Annaler: Series A, Physical Geography. 86 (4): 385–400. doi:10.1111/j.0435-3676.2004.00239.x. ISSN 0435-3676. S2CID 128954456. Archived from the original on 2013-01-05.