Carpathian Mountains

Definition and stakes

Oscar Briliant and Philip Lake,  1911 Encyclopædia Britannica, Volume 5… (1911)

“ The Carpathians, which only in a few places attain an altitude of over 8000 ft., lack the bold peaks, the extensive snow-fields, the large glaciers, the high waterfalls and the numerous large lakes which are found in the Alps. They are nowhere covered by perpetual snow, and glaciers do not exist, so that the Carpathians, even in their highest altitude, recall the middle region of the Alps, with which, however, they have many points in common as regards appearance, structure and flora. ”
Source: Wikisource

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“ The Carpathian range of mountains stretches from the northwest along the north and down the east, encircling the lowlands and sending forth rivers and streams to water the plains. These mountains are of a gigantic bulk and breadth; they are covered with fir and pine trees, and in the lower regions with oaks and many other kinds. The peaks of the high Tátra are about 9,000 feet high, and, of course, are bare of any vegetation, being snow-covered even in summer-time. On the well-sheltered sides of these mountains numerous baths are to be found, and they abound in mineral waters. ”
Source: Gutenberg

Oscar Briliant and Philip Lake,  1911 Encyclopædia Britannica, Volume 5… (1911)

“ The inner zone is not continuous, and is much more complex in structure. It is visible only in the west and in the east, while in the central Carpathians, between the Hernad and the headwaters of the Theiss, it is lost beneath the modern deposits of the Hungarian plain. In the western Carpathians the inner zone consists of a foundation of Carboniferous and older rocks, which were folded and denuded before the deposition of the succeeding strata. In the outer portion of the zone the Permian and Mesozoic beds are crushed and folded against the core of ancient rocks ”
Source: Wikisource

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