| 词条 | Geology of Monaco |
| 释义 |
The geology of Monaco is closely related to the end of the Western Alps, forming the small country's steep corniche coastline. During the last 2.5 million years of the Quaternary high sea levels between glaciations formed erosion terraces and left behind coastal sediment deposits. Beach sands are mixed with frost chippings and other cold-weather remnants of the glacial period and preserve large mammal remains and archaeological remains of early humans in the Gîte des Moulins Cave and the Jardin Exotique. Monaco hosts the International Hydrographic Organization. [1] References1. ^{{cite book |author=Moores, E.M.; Fairbridge, Rhodes W.|year=1997|title=Encyclopedia of European & Asian Regional Geology|publisher=Springer|p=540}} {{Europe topic|Geology of}} 2 : Geology of Monaco|Geology by country |
| 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。