Search results
Results From The WOW.Com Content Network
Tombolo near Karystos, Euboea, Greece Tombolo contrasted with other coastal landforms.. A tombolo is a sandy or shingle isthmus.A tombolo, from the Italian tombolo, meaning 'pillow' or 'cushion', and sometimes translated incorrectly as ayre (an ayre is a shingle beach of any kind), is a deposition landform by which an island becomes attached to the mainland by a narrow piece of land such as a ...
In the case of a cuspate foreland that has formed close to an island, it is possible for it to extend right up to the island, forming a tombolo. [1] Depending on the physical conditions such as storms, the feature can alternate between a cuspate foreland and a tombolo. [1] Gabo Island in South Australia is an example of where this occurs. [1]
This list of isthmuses is an appendix to the article isthmus.The list is sorted by the region of the world in which the isthmus is located. An isthmus (/ ˈ ɪ s θ m ə s / or / ˈ ɪ s m ə s /; plural: isthmuses, or occasionally isthmi; from Ancient Greek: ἰσθμός, romanized: isthmos, lit.
The sandy isthmus or tombolo "The Neck" connects North and South Bruny Island in Tasmania, Australia. An isthmus (/ ˈ ɪ s m ə s, ˈ ɪ s θ m ə s /; [1] pl.: isthmuses or isthmi) [2] is a narrow piece of land connecting two larger areas across an expanse of water by which they are otherwise separated. [3]
Tombolo seen from Dogashima Park. Tombolo is a shingle isthmus that connects Dogashima with the Sanshiro Islands at low tide.Tombolo is named after the Italian word tombolo, meaning 'pillow' or 'cushion', which refers to a deposition landform by which an island becomes attached to the mainland by a narrow piece of land such as a spit or bar.
Main page; Contents; Current events; Random article; About Wikipedia; Contact us
The Murihiku terrane was formed in Late Triassic to Late Jurassic times (220–145 Ma). [ 2 ] A line of Dun Mountain–Maitai terrane rocks pass NNW–SSE through the centre of the Northland region, separating the Murihiku terrane from the more easterly terranes, and produce a detectable junction magnetic anomaly (JMA), but do not crop out.
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.