Agriculture
The South of England has a lot of gardens and orchards. People grow apples, pears, cherries, plums and other fruits and different berries there. But many parts of highland Britain have only thin, poor soils. In most of these areas the farmers have cultivated only valley lands and the plains where the soils are deeper and richer.
Farming land is divided into fields by hedges or stone walls. Most of countryside England is agricultural land, about a third of which is arable and the rest is pasture.
Sheep-, cattle- and dairy-farming are also important branches of Great Britain’s economy. Chicken farms produce a great number of chickens and eggs for the population. Great Britain produces a lot of wool. Woollen industry is developed in Yorkshire. British woollen products are exported to other countries.
Примечание: подробнее о развитии животноводства в США читайте текст “Farms in the USA” (ex. 12, стр. 23 – 24, Lesson 5, «Методические разработки на английском языке по курсу «Животноводство», часть 1).
The United States of America Geographical Position
The United States territory consists of three separate parts, different in size, natural features, level of development and population:
1) the main part, the United States proper, with an area of 7,800,000 square kilometres. It borders on Canada in the north and on Mexico in the south. It is washed by the Pacific Ocean in the west, the Atlantic Ocean in the east, and the Gulf of Mexico in the south-east;
2) Alaska, which occupies the north-western part of the continent of North America, including a lot of islands;
3) Hawaii in the Pacific Ocean.
Coasts
The coastline length of the United States proper is 22,860 km. The Atlantic coast is mostly lowland and greatly indented. The Pacific coast is mountainous, in the northern part cut by numerous fiords.
Relief
About half the United States’ territory is covered by plateaus and mountains.
The eastern part of the country is occupied by the Appalachian Mountains, which in the north come close to the Atlantic coast and in the south are separated from it by the Atlantic Lowland.
West of the Appalachians stretch the Central Plains, the Great Plains, and the Mexican Lowland.
The Central Plains are 500 – 400 m high and have a hilly moraine relief in the north and a more gentle erosional relief in the middle and southern parts.
The Great Plains (west of west longitudes 97 - 98°) are a deeply cut plateau with the heights of 500 m in the east to 1600 m at the Cordillera foothills.
The flat Mexican Lowland, with the height of up to 150 m, is swampy along the Gulf coast and fringed by a strip of marsches.
The western part of the country (including almost the whole of Alaska) is made up of high mountain ranges, tablelands and plateaus of the Cordillera system.
The Cordilleras consist of rows of mountain ranges with the heights of up to 3000 – 5000 m and a broad strip of intermountain tablelands and plateaus. In Alaska the mountain ranges stretch in the west-east direction and include the Brooks Range, the Yukon Tableland, the Aleutian Range with Mount McKinley, 6193 m – the highest peak of the USA and the whole of North America.
On the territory of the USA proper the mountain ranges stretch in the north-south direction. The first from the east are the Rocky Mountains, reaching up to nearly 4400 m. West of the Rockies lie vast plateaus and tablelands: the volcanic Columbia Plateau, the Great Basin – a desert tableland with deep depressions (the largest is the Death Valley, containing the lowest point in the western hemisphere – 86 m below sea level), the Colorado Plateau. Typical for this area is the alternation of tablelands situated at the height of about 2000 m and mountain ranges reaching up to 3000 – 5000 m, with numerous deep river canyons.
Further west is a narrow belt of the Cascade Mountains, and the Sierra Nevada Range (over 4400 m). Still further west lies an area of valleys (Willamette, the Californian Valley).
The Pacific coast is formed by the deeply cut Coastal Ranges with the height of up to 2400 m.