| 词条 | Lansdowne Bank |
| 释义 |
Lansdowne Bank, sometimes called Landsdowne Bank, is an extensive submerged bank located between the main island of New Caledonia and the Chesterfield Islands, in the easternmost part of the Coral Sea. It covers an area of {{convert|4,300|km2|0|abbr=on}},[1] making it one of the largest banks of the world, has general depths of {{convert|60|to(-)|80|m|0|abbr=out}}, and a largely sandy bottom. Two reefs mark the shallowest spots of the bank, but they are still submerged at low tide. Fairway Ridge, also called Fairway Plateau, is a submarine feature shown on some maps in that area. The Lansdowne Bank area marked is far larger than Fairway Plateau, but there are smaller, unnamed plateaus nearby. The Lansdowne Bank area, shown at the northeastern end of Lord Howe Rise, is separated from New Caledonia by New Caledonia Basin and Fairway Basin. Nereus ReefNereus Reef is at the northern end of Lansdowne Bank. Its given position of {{coord|20|07|S|160|28|E|name=Nereus Reef}} is doubtful.[2] Nereus Reef has the least depth of the bank, with {{convert|3.7|m|ft}}. A shoal with a depth of {{convert|16|m|ft}} is {{convert|14|mi|km|0}} west-northwest of Nereus Reef. Fairway ReefThe southeastern end of Lansdowne Bank is marked by Fairway Reef, thus named from its lying in the fairway between Australia and New Caledonia, midway between the Bellona Reefs (south of the Chesterfield Islands) and New Caledonia. Fairway Reef is {{convert|3.2|km|mi}} long, about 4 to 5 fathoms (7.3 to 9.1 metres) deep, of coral bottom, and located at {{coord|21|00|15|S|161|45|09|E|name=Fairway Reef}}. According to some sources, Fairway Reef dries at low tide.[3] Sandy Island MysteryGoogle Maps and other internet maps showed a large landmass named Sandy Island in northern Lansdowne Bank, but did not show an image for it. The non-existence of this phantom island had been proved by French missions in the 1970s, and the information passed to hydrographic services around the world, but it had remained in the World Vector Shoreline Database. In 2012 Australian scientists again proved the island does not exist.[4][5]See also
References1. ^Le parc naturel de la mer de Corail, p. 26 2. ^{{cite book | last = | first = | authorlink = | title =Publication 127: Sailing Directions (Enroute): East Coast of Australia and New Zealand | publisher =National Geospatial Intelligence Agency (NGA) | series = | volume = | edition =8 | year =2004 | location =Bethesda, Maryland | page =135 | url =http://permanent.access.gpo.gov/websites/pollux/pollux.nss.nima.mil/NAV_PUBS/SD/pub127/127sec06.pdf |format=PDF | doi = | id = | isbn = }} 3. ^{{cite web | last = | first = | authorlink = | coauthors = | title =Reefbase: A Global Information System for Coral Reefs | work = | publisher =WorldFish | date =April 2013 | url =http://www.reefbase.org/global_database/default.aspx?section=r1®ion=22&country=NCL | format = | doi = | accessdate = 2013-04-19 }} 4. ^{{cite web | title = South Pacific Sandy Island 'proven not to exist' | url = https://www.bbc.co.uk/news/world-asia-20442487 | work=BBC News | date = 22 November 2012 | accessdate = 22 November 2012}} 5. ^{{cite web |url=https://www.theguardian.com/world/2012/nov/22/sandy-island-missing-google-earth |title=The Pacific island that never was |work=The Guardian |date=22 November 2012 |accessdate=22 November 2012}} External links
3 : Landforms of New Caledonia|Coral reefs|Undersea banks of the Pacific Ocean |
| 随便看 |
开放百科全书收录14589846条英语、德语、日语等多语种百科知识，基本涵盖了大多数领域的百科知识，是一部内容自由、开放的电子版国际百科全书。