Tombolo: Difference between revisions
Jump to navigation
Jump to search
Pat Palmer (talk | contribs) mNo edit summary |
Pat Palmer (talk | contribs) mNo edit summary |
||
Line 8: | Line 8: | ||
==References== | ==References== | ||
{{Reflist|refs= | {{Reflist|refs= | ||
<ref name=Mahiques> | <ref name=Mahiques> | ||
{{Cite book | {{Cite book | ||
Line 24: | Line 25: | ||
}} | }} | ||
</ref> | </ref> | ||
}} | }} |
Revision as of 07:28, 11 March 2024


An example of a tombolo seen from the air. This one is on cape Paximadhi in Greece.
Tombolo is the geographic term for an isthmus (narrow neck connecting an island to a land mass) formed when currents carrying sand are slowed by an island, depositing a sandbar that transforms the island into a peninsula.[1]
Presqu'ile (Ontario) is an example of a tombolo.
References
- ↑ Michel Michaelovitch De Mahiques (2016). “Tombolo”, Encyclopedia of Estuaries, 713–714. DOI:10.1007/978-94-017-8801-4_349. ISBN 978-94-017-8800-7.