Physical characteristic

Canada takes the second place after Russia for the area; it occupies 9985 thousand km². Canada stretches from the north to the south to 4600 km; from the west to the east to 5100 km. It extends from the Atlantic to the Pacific and northward into the Arctic Ocean.

Boreal forests prevail on the rocky Canadian Shield, while ice and tundra are prominent in the Arctic. Glaciers are visible in the Canadian Rockies and Coast Mountains. The flat and fertile prairies facilitate agriculture. The Great Lakes feed the St. Lawrence River in the southeast, where lowlands host much of Canada's population.

Average winter and summer high temperatures across Canada vary from region to region. Winters can be harsh in many parts of the country, particularly in the interior and Prairie provinces, which experience a continental climate, where daily average temperatures are near −15 °C, but can drop below −40 °C with severe wind chills. In noncoastal regions, snow can cover the ground for almost six months of the year, while in parts of the north snow can persist year-round. Coastal British Columbia has a temperate climate, with a mild and rainy winter. On the east and west coasts, average high temperatures are generally in the low 20s °C, while between the coasts, the average summer high temperature ranges from 25 to 30 °C.

Читайте також:

<== попередня сторінка	\|	наступна сторінка ==>
Lesson 13	\|	Political system

Не знайшли потрібну інформацію? Скористайтесь пошуком google:

Генерація сторінки за: 0.002 сек.