Languages
In the European continent exist several languages with different origins. Among them we emphasized:
Of the Latin, Romance languages: Castilian or Spanish, French, occitano, Sardinian, Italian, Rumanian, Portuguese, Asturian, Galician, Catalan, retorrománico (grisón or Romance) and francoprovenzal.
Germanic languages: English, Dutch, German, under sajonés, Frisian, Swedish, Danish, Norwegian, Icelandic, Scottish, feroés
Slavic: Bosnian, Bulgarian, Russian, Pole, Czech, bielorruso, ucraniano, sorabo, serbocroata, Slovene and Macedonian.
Of the group ugro-Finn: Hungarian, Finn and estonio.
Of the céltico: Irish, gaélico Scot, Welshman, bretón, córnico and manés.
Greek.
Of the group the Baltic Sea: letón, lituano.
Of Asian origin: Albanian
Turkish
Basque
Lapón.
The five used languages more are the English, the French, the German, the Russian and the Italian.

Climate
The European continent is a to a large extent tempered zone.
Its nonsingle climate also varies of north to the south but of the west to this because of continental marine and continental the marine and polar tropical airflow and airflows polar, to a lesser extent tropical.
In Europe we can distinguish the following types climates:

Mediterranean climate
Between 30º and 45º of latitude can be found the climate Mediterranean. Of him it is possible to emphasize the dryness that take place during the summer caused by the subtropical anticyclone, and the humidity of the winter due to the polar front. The air masses that are are of marine marine or continental and polar type tropical. The temperatures are smooth, since during the year as soon as they vary about 15 ºC.

Oceanic climate
It is a climate that includes/understands the borders of the Atlantic Ocean and goes from Norway to the Portuguese North coast. It has a constant humidity and moderate temperatures without great oscillations, which increase of the west to this, when increasing the continentalidad. The abundant precipitations also diminish towards the east, and in general they are superior to 1000 mm annual with maximums in the winter.

Mediterranean climate
Continental climate One characterizes by the resistance between precipitations and discharges temperatures of the summer, and the cold dryness of the winter. The high temperatures of the summer cause that the evaporation of the water that falls in shower form is very high. Climate of tundra One occurs between the 60 and 80 degrees of latitude, in Europa.Se it throughout characterizes by little precipitations and a constant cold with 10 principles of ºC the year. This causes that the water is accumulated in quagmires and an ice layer is created in the ground that maintains it little of nutrients and with a low biodiversity.

Mountain climates
In the mountain climate the temperature diminishes of 0.5 to 1ºC with each 100 meters of height, which increases the humidity relative of the air and causes precipitations. This mountain climate is characterized to have special winds and a greater exhibition to the sun, which it difference of the zonal climate in which encuentra.Las temperatures are smooth, since during the about 15 year as soon as they vary ºC.

Oceanic climate
It is a climate that includes/understands the borders of the Atlantic Ocean and goes from Norway to the Portuguese North coast. It has a constant humidity and moderate temperatures without great oscillations, which increase of the west to this, when increasing the continentalidad. The abundant precipitations also diminish towards the east, and in general they are superior to 1000 mm annual with maximums in the winter.