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Veľká Fatra
Veľká Fatra (also Great Fatra or Greater Fatra) is a mountain range in the Western Carpathians in Slovakia.〔''Lonely Planet Czech & Slovak Republics'' Lisa Dunford, Brett Atkinson - 2010 Page 57 "Central Slovakia ranges include the Low Tatras, reaching about 2000m, and the Malá Fatra and Veľká Fatra."〕 The Veľká Fatra lie to the southwest of the better known Malá (Lesser) Fatra mountains and are less developed, as well as, contrary to the name, being lower.〔''Lonely Planet Czech & Slovak Republics'' Lisa Dunford, Brett Atkinson - 2010 Page 310 "To the southwest the Veľká (Greater) Fatra mountains are far less popular and developed (and contrary to logic, lower than the Malá Fatra)."〕
==Geology==
In the geomorphological system, it is a part of the Fatra-Tatra Area. It is situated approximately among the towns of Ružomberok, Harmanec, Turčianske Teplice and Martin. The Turiec Basin and the Lesser Fatra mountains are situated to the north west of the range and the Low Tatras mountains are in the east. It can be divided into seven parts: ''Šípska Fatra, Šiprúň, Lysec, Hôľna Fatra, Revúcke podolie, Zvolen and Bralná Fatra''.
The highest mountain is Ostredok at . Other notable summits of the largest ''Hôľna Fatra'' part are Krížna at and Ploská at , where the main ridge divides into two. The western Turiec Ridge ((スロバキア語:Turčiansky hrebeň)) includes, for example, Borišov at , and the eastern Liptov Ridge ((スロバキア語:Liptovský hrebeň)) includes, for example, Rakytov at . ''Bralná Fatra'' includes Tlstá at and Ostrá at summits. The Zvolen massif () connects the Veľká Fatra Range with the Low Tatra Range. One of the largest ski resorts in Slovakia - Skipark Ružomberok and Donovaly - lies beneath it. There are several other tourist and skiing resorts in the range.
A considerable part of the range is made of various Mesozoic rocks. The central part and the main ridge are made up of non-resistant rocks (slates) and the relief is softly modeled (Ploská, Ostredok). The southern and south-western part is formed by resistant limestone and dolomite with rocky walls and reefs. The ridges are usually separated by canyon-like valleys. The most important ones are Gader Valley (''Gaderská dolina'') and Blatnica Valley (''Blatnická dolina''). The longest valley is the Ľubochňa Valley (''Ľubochnianska dolina'') at 25 km. Numerous karst formations are located in this area and the Harmanec Cave is one of the best known caves in Slovakia.
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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