Search results
Results from the WOW.Com Content Network
Winters in Albania are characteristically mild and wet while summers are warm and dry. The northern areas of country such as the Albanian Alps experiences a subarctic climate with frequently very cold winters, and short, mild summers. The lowlands of Albania have mild winters, averaging about 7 °C (45 °F). The summer temperatures average 32 ...
An enlargeable topographic map of Albania. Geography of Albania. Albania is: a country; Location: Eastern Hemisphere; Northern Hemisphere. Eurasia. Europe. Southern Europe. Balkans (also known as "Southeastern Europe") Time zone: Central European Time , Central European Summer Time ; Extreme points of Albania. High: Maja e Korabit 2,764 m ...
Albania (/ æ l ˈ b eɪ n i ə, ɔː l ... (24 and 118 inches) depending on geographical location. [143] The northwestern and southeastern highlands receive the ...
Northern Albania or Ghegeria (Gheg Albanians) Southern Albania or Toskeria (Tosk Albanians) In tourism geography, Albania can be divided into three regions: Coastal Albania – the long narrow strip between about 10 and 30 km wide along the whole Albanian coast, bordering both the Adriatic Sea and Ionian Sea. Albanian Adriatic Sea Coast
You are free: to share – to copy, distribute and transmit the work; to remix – to adapt the work; Under the following conditions: attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made.
Topographical map of Albania. The Northern Mountain Region (Albanian: Krahina Malore Veriore) is a geographical region in northern Albania. [1] It is one of the four mountain regions of Albania, the others being Central Mountain Range, Southern Mountain Range, and Western Lowlands.
Albania geography-related lists (1 C, 19 P) A. Albanian Adriatic Sea Coast (17 P) Albanian Ionian Sea Coast (30 P) Albanian Ohrid Lake Coast (5 P) B. Borders of ...
Tectonic Map of Albania Source: Ministry of Mines and Energy Resources (1999) Albania is mostly mountainous, with the first alpine regions forming towards the end of the Jurassic period. During the Cenozoic era, the malformation of the Albanides accelerated, causing the subterranean landscape to take its present form.