Lataretu catalin Muntii Fagaras

Muntii Fagaras

Student : Lataretu Catalin Ionut

Group:8212

English Project

MUNŢII FĂGĂRAŞ

-the highest peaks of the Romanian Carpathians;-the longest Carpathian ridge (about 70km.) heights  always exceeding 2000 meters elevation.

Valea S

ambata

Since July 2011 Chalet Valley Sambetei things began to change for the better, with a new chalet cottage, Mr. Nae Zdraila, former chalet Chalet in Bucegi Malaiesti.

Depresiunea Făgăraş

Depresiunea Fagaras, also known as the "Land of Fagaras" or "Olt Country" is a depression of erosion, located in the central part of Romania, in the southern edge of the hills of Transylvania Depression, entering into direct contact with Fagaras mountains.

Şaua Portiţa Viştei 2130mspre valea Viştea Mare

Refugiul alpin Viştea Mare

Vf. Viştea Mare2527m.

Vf. Moldoveanu 2544m

The limit of the forest (coniferous)and alpine area

Vf. MoldoveanuMoldoveanu Peak is the highest mountain peak in Romania, located in Fagaras Mountains, Arges county. Its altitude is 2,544 meters. Because of its surrounding mountain peaks, most of over 2,400 meters, Moldoveanu peak is visible only from Fagaras ridge or in the air, unlike many of the major peaks of the chain Fagarasanul that are visible from Fagaras Depression.

In the Pleistocen climate cooling caused globe at an altitude of 1800-2000 m., In the Carpathian area, the emergence of the present situation of permanent snow.? For this reason there has been a large amount of snow accumulation and its gradual transformation into ice - Carpathian glaciation - which led sculpting glacial cirques, storage places. ?? In Holocene climate warming has resulted in glaciers, so the glacier were occupied by water and glacial lakes were formed.

Vale glaciară

Once the icewas accumulated in amountsLarge began the process of"Flow" of it, havingplace the genesis of glacial valleys withtheir specific shape of the letter "U".

Vale glaciară

The valley is a negative form of relief, narrow and elongated, with decreasing downstream slope created by the action of various forms of flowing water. It appears as a depression or hollow elongated land, crossed (permanently or temporarily) by a river. It may be a lowland region located below the surrounding lands and watered by a river.

Vf. Moldoveanu 2544m.Vf. Viştea Mare

Masses of debris at the footslope, "sea of rocks"

Crossing a strip of hardened snowend of July

The world is a book, and those who do not travel, read only a page.

www.nature.com

www.romania.info/ro/tags/fagaras

Bibliography