Tied island
Tied islands or land-tied islands are landforms consisting of an island that is connected to the mainland or another island only by a tombolo: a spit of beach materials connected to land at both ends.[1][2] St Ninian's Isle in the Shetland Islands off the north coast of Scotland is an example: it was once an island but is now linked to the mainland.
Other examples include Maury Island, Washington in Puget Sound, Coronado, California, and Nahant, Massachusetts in the United States; Paraguana Peninsula in Venezuela; Barrenjoey, New South Wales and Wedge Island, Western Australia; Paratutae Island in New Zealand; Mount Hakodate in Japan, Howth Head in Ireland; Davaar Island, Campbeltown, Scotland; Chefoo island in Yantai, China; and Cheung Chau in Hong Kong.
The Isle of Portland, in England, is also described as a tied island, but geographers now believe that Chesil Beach, which connects the island to the mainland, is a barrier beach that has moved eastwards, rather than a tombolo, which would have been formed by the effect of the island on waves.
Paniquian Island, also known as Isla Boquete, is a small tied island in Puerto Galera, a popular tourist destination in the Philippines. The island is connected to the main island of Mindoro by a small tombolo, which is submerged only a few times per year.
See also
[edit]- Presque-isle – Peninsula with narrow connection to mainland (name from French for "almost island")
- Peninsula – Landform surrounded more than half but not entirely by water
- Tidal island – Island accessible by foot at low tide
Islands portal
References
[edit]- ^ "What Is a Tied Island?". WorldAtlas. May 11, 2018.
- ^ "Definition of TIED ISLAND". www.merriam-webster.com.
- Glossary of geology and related sciences. Jesse V. Howell, American Geological Institute. 1962.
- Some Coastal Landform Definitions. Matthew Flinders, Villanova College, Queensland.
External links
[edit]Media related to Tied islands at Wikimedia Commons