翻訳と辞書 Words near each other ・ Matjaž Mulej ・ Matjaž Perc ・ Matjaž Pograjc ・ Matjaž Pungertar ・ Matjaž Rozman ・ Matjaž Schmidt ・ Matjaž Sekelj ・ Matjaž Smodiš ・ Matjaž Vrhovnik ・ Matjaž Zupan ・ Matjaž Šinkovec ・ Matjhabeng Local Municipality ・ Matjiesfontein ・ Matjiesrivier ・ MATK ・ Matk Combe ・ Matka ・ Matka Canyon ・ Matka gambling ・ Matka Joanna ・ Matka-class missile boat ・ Matka-ye Rudbar ・ Matkah Point ・ Matkahuolto ・ Matkalla Porkkalaan ・ Matke ・ Matki (disambiguation) ・ Matki (earthen pot) ・ Matki Dance ・ Matki, Iran Dictionary Lists mini英和辞書 mini和英辞書 Webster 1913 Latin-English FOLDOC Wikipedia English ウィキペディア

翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Matk Combe ： ウィキペディア英語版 Matk Combe The Matk Combe ((スロベニア語:Matkov kot)), in older sources also the Jezera Valley (''dolina Jezera'')〔Seidl, Ferdinand. 1907. ''Kamniske ali Savinjske Alpe, njih zgradba in njih lice''. Ljubljana: Matica Slovenska, p. 17.〕 is an Alpine glacial valley in Slovenia. ==Geography== The Matk Combe lies in the upper catchment area of the Savinja River〔Natek, Karel. 1992. ''Discover Slovenia''. Ljubljana: Cankarjeva založba, p. 14.〕 in the Kamnik–Savinja Alps of Slovenia. The valley floor ranges between and in elevation.It is surrounded by high mountains to the southwest, from Cold Mountain ((スロベニア語:Mrzla gora), ) to the west to Mount Savinjka () to the east. The border between Slovenia and Austria runs along the western ridge, and to the east it borders the Logar Valley. The Matk Combe is relatively remote and difficult to reach. There is a forest road into it from the Logar Valley, which also connects the farms in it. At the bottom of the valley, this road branches off from the road leading to the former border crossing at the Pavlič Pass ((スロベニア語:Pavličevo sedlo), (ドイツ語:Pavlitschsattel); ) in the Karawanks. The valley is about long and has the most characteristic glacial features in its upper half. Below Cold Mountain in the southwest part of the valley there are well-formed cirques. The eastern ridge above the valley consists of solid dolomite. The southern part of the valley consists of Triassic limestone, and it is only in the north that late Paleozoic impermeable rock is exposed, which is already part of the Karawanks. The valley floor spreads out only in the upper part of the combe. The valley floor is filled by gravel carried by flashy streams and glacial moraines. Jezera Creek has its source in the middle of the valley; below its spring it has carved out and narrowed the valley, creating the picturesque Lamotje Gorge in the limestone rock where it enters the Logar Valley. During the Pleistocene the valley was filled by a glacier that extended to the Logar Valley and joined the glacier there. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Matk Combe」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.