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Physical Characteristics The Great Plains meet the Rocky Mountains in Wyoming. The state is a great plateau broken by a number of important mountain ranges. In the northwest are the Absaroka, the Owl Creek, Wyoming, Gros Ventre, Wind River and the Teton ranges.
The State is considered semiarid east of the mountains. There are several mountain ranges, but the mountains themselves cover less area than the high plains. The topography and variations in elevation make it difficult to divide the State into homogeneous, climatological areas.
Did you know that Wyoming has the second highest average elevation in the United States? This is thanks to the many stunning mountain ranges that span the state.
Climate of Wyoming. Wyoming's climate is influenced by its interior location on the North American landmass and by its high mean elevation. The state includes areas of arid desert, semiarid steppe (short-grass prairie), and alpine climates.
Rural subdivision and development, energy development, invasive species, climate change, and disruption of historic disturbance regimes are five important conservation issues that extend across a majority of Wyoming's habitat types and wildlife species.
State and local governments can adopt more stringent laws and regulations than allowed under federal law, unless prohibited by federal statute. For example, many states have enacted more stringent air emission standards and requirements than are imposed by federal laws.
Since 1973, the Wyoming Department of Environmental Quality (DEQ) has served as the state's regulatory agency charged with protecting, conserving and enhancing Wyoming's land, air and water for the benefit of current and future generations.
The state includes areas of arid desert, semiarid steppe (short-grass prairie), and alpine climates. The arid desert regions are all found in the western half of the state and have average annual rates of precipitation of between about 4 and 8 inches (100 and 200 mm).