A wide variety of wildlife is found throughout the Interior Plains region. Some of the animals include mule deer, pronghorn antelope, brown bear, wolf and elk. These animals make this region their home because of the abundance of space and food there.
Inner Lowlands Undulating flat country with many rivers, wide river valleys and grassy hills.
Most trees are deciduous. In the southern Interior Plains, the natural vegetation consists mainly of grasses. In the northern part of the Interior Plains only small plants, mosses and grasses grow.
The Interior Plains are rich in natural resources such as oil, minerals and fertile soil. These resources have helped this region develop mining, agriculture and other primary industries.
In the Interior Plains there are igneous, sedimentary and metamorphic rocks. They formed when soils were deposited from the Canadian Shield rivers and sedimentary rocks were formed horizontally from these deposits. These deposits created large areas of flat land, river valleys, and rolling hills.
Lowlands, rolling hills, lakes, rivers and some of the most fertile soils in the world are all present in the region. There are three sub-regions in the interior lowlands: the Interior Plains, the Great Plains, and the Canadian Shield.
In the United States, the Great Plains include portions of 10 states: Montana, North Dakota, South Dakota, Wyoming, Nebraska, Kansas, Colorado, Oklahoma, Texas, and New Mexico. p>
The Interior Lowland stretches from the Gulf of Mexico in the south to Hudson Bay in the north. While the southern and eastern portions of the eastern lowlands consist of the Gulf and Atlantic coastal plains winding around the eastern mountains in a gradual slope towards the sea.
The climate of the Interior Plains varies greatly. The weather is very extreme; In the north, winters are long and summers are short and cool, and in the south, summers are long and hot and winters are cold, but there is very little rainfall.
The central-south area of the Interior Plains has a typical continental climate – very cold winters, hot summers, and relatively little rainfall.
A series of tectonic plate collisions in the crust that formed the center of the North American continent laid the foundations for today’s inner plains. Mountain building and erosion around the plains, as well as flooding from inland seas, provided sediments that make up the rock strata of the inner plains.
In the inner plains, the forest merges with the grassland to create an arc of aspen parkland characterized by prairie vegetation interspersed with groves of trembling (trembling) aspen and other poplar species in areas with low humidity and along valley bottoms.
The Interior Plains region of Canada was once covered with many different types of grass. Today’s vegetation consists of grasses with long roots such as bluegrass, June grass and hedgehog grass as well as pine, spruce and fir trees. This vegetation grows here because many farmers grow oats, barley, wheat and more crops.
Large areas of luvian soils occur in the central to northern Interior Plains; smaller areas in all regions south of the permafrost zone. The 2 major groups of luvian soils are distinguished mainly by soil temperature.
You will notice that this entire region is generally flat. Just like the Cordillera, the human population in the Southern Plains Region tends to be larger, but you’ll also find that cities and towns are generally attached to a water source such as a lake or river.
There are a large majority of waterways in the Interior Plains, including Lake Winnipeg, Great Bear Lake, Great Slave Lake, and Lake Manitoba. The Interior Plains consist of deep, fertile soil due to the waterways and overall rainfall.
Canada can be divided into seven physiographic regions: Arctic Lands, Cordillera, Interior Plains, Hudson Bay Lowland, Canadian Shield Forest Lands, St Lawrence Lowlands and Appalachia. The divisions are based on the relatively similar physical geography and landforms of each area.
The Interior Plains is a large region that includes parts of Manitoba, Saskatchewan and Alberta, as well as parts of the Northwest Territories and the Yukon Territory. This region is rather flat, with low hills. It has grasslands, wooded parklands and large northern forests.