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The Rucăr-Bran Pass. The Rucăr–Bran Pass, also called in English the Bran Pass (German: Törzburger Pass, Hungarian: Törcsvári-szoros), is a mountain pass in Romania, linking the counties of Brașov and Argeș.
The Bucegi Natural Park with an area of 32.663 ha [3] was declared a protected area by Law Number 5 of March 6, 2000 (published in Monitorul Oficial Number 152 of April 12, 2000) [4] and represents a mountainous area (caves, pit caves, canyons, ridges, sinkholes, valleys, waterfalls, pastures and forests), that shelters a variety of flora and fauna.
File:Bucegi Mountains, Romania.jpg cropped 44 % horizontally, 37 % vertically, 65 % areawise using CropTool with precise mode. File usage The following page uses this file:
[1] To the east, the Bucegi Mountains have a very steep slope towards the popular tourist destinations in the Prahova Valley, such as Bușteni and Sinaia. At a higher elevation is the Bucegi Plateau, where wind and rain have turned the rocks into spectacular figures such as the Sphinx and Babele.
Sphinx from Bucegi. The Sphinx (Romanian: Sfinxul) is a natural rock formation in the Bucegi Natural Park which is in the Bucegi Mountains of Romania. It is located at an altitude of 2,216 metres (7,270 ft) within the Babele complex of rock formations. The first photo of the Great Bucegi Sphinx was probably taken in about the year 1900. This ...
Ceahlău - "Piatra Lată din Ghedeon" rock formation Leontopodium alpinum, edelweiss or floare de colț is a protected species in Romania since 1933. Ceahlău National Park shelters a large variety of flora and fauna; some of the species are endemic or rarely seen elsewhere in Romania.
Josh McDaniels is headed back to New England for a third stint as the Patriots' offensive coordinator. Here's why the Patriots hired him:
Babele (meaning The old women) is the name for an area on the Bucegi Mountains plateau in Romania, within the Southern Carpathians. [1] Babele is one of the most popular tourist destinations in the country. The name comes from some mushroom shaped rock formations, the result of erosion and varying hardness of the rock layers.