Geography
Pennsylvania is known for its diverse geography, which includes mountains, forests, valleys, and rolling hills. The state is divided into three main geographic regions: the Appalachian Mountains, the Allegheny Plateau, and the Atlantic Coastal Plain.
The Appalachian Mountains run through the central part of Pennsylvania. The highest point in the state is Mount Davis, which rises to 3,213 feet (979 meters) above sea level. The Appalachian Mountains are a major source of water for Pennsylvania, and they are also home to several ski resorts and hiking trails.
The Allegheny Plateau covers the western and northern parts of Pennsylvania. This region is characterized by its rolling hills and valleys. The Allegheny Plateau is home to several natural gas and coal deposits, and it is also a major dairy farming region.
The Atlantic Coastal Plain covers the southeastern part of Pennsylvania. This region is characterized by its flat terrain and sandy soil. The Atlantic Coastal Plain is home to several major cities, including Philadelphia and Pittsburgh.
Climate
Pennsylvania has a humid continental climate, with four distinct seasons. The summers are hot and humid, with average temperatures in July ranging from 70 to 80 degrees Fahrenheit (21 to 27 degrees Celsius). The winters are cold and snowy, with average temperatures in January ranging from 20 to 30 degrees Fahrenheit (-7 to -1 degrees Celsius).
Pennsylvania receives an average of 43 inches (109 centimeters) of precipitation per year. The precipitation is evenly distributed throughout the year, although there is a slight peak in the summer months.
The climate of Pennsylvania varies slightly from region to region. The mountainous regions of the state are cooler and more humid than the coastal regions. The western part of the state is also slightly drier than the eastern part.
