Tarcu Mountains and Bistra Lake, relief and description, more info

Tarcu Mountains and Bistra Lake, relief and description, more info

Tarcu mountainous terrain can be likened to a vast amphitheater in the Banat neighborhood plain and composed largely of three steps. The highest consists of peaks over l800-2000 m height, located in the south-east to Hideg, Ses River and Great River / Mare River. It is characterized by smooth, ice buckets lined peaks and alpine meadows stretched. This stage includes four massive high mountains that make up Tarcu Mountains group, namely the massive Tarcu, Bloju and Small Mountain / Mic Mountain.

In the middle level falling heights 1100-1500 m, making up an area that surrounds the west and north the previous one. Distinguished Peak High Glade / Varful Poiana Inalta, near Hideg, Peak Plesii and on the north side of the mountains, Magura Hillock / Magura Marga and Clopotivei.

Lowest step, with heights of 500-800 m, is in contact with Caransebes Depression and reaches a width of 2-3 km.
From geological point of view, Tarcu Mountains are composed of granite (Bloju Massive, Petreanu Massive and Small Mount Massive / Mount Mic) surrounded by crystalline schists and sedimentary rocks (sandstone, tuffs, conglomerates etc.), especially in their part of the southeast. Hard crystalline schists and gneisses for Tarcu Peak and Prislop Peak, generally, highest relief consists of crystalline schists and granite.
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