Lakes & Ponds
An inland body of standing water is called a lake or a pond. It can be as small as a few square meters or as large as thousands of square meters. Some ponds might be filled with water for only a few weeks or months each year, whereas some lakes have existed for thousands of years. In temperate regions, the temperature of lakes and ponds varies depending on the season.
During the winter, most of the water in a lake or pond is the same temperature. In the summer, the warmer water on top is less dense than the colder water at the bottom. During the spring and fall, as the water warms or cools, turnover occurs. The top and bottom layers of water mix, often due to winds, and this results in a uniform water temperature. This mixing circulates oxygen and brings nutrients from the bottom to the surface.
Nutrient-poor lakes, called oligotrophic lakes, often are found high in the mountains. Few plant and animal species are present as a result of small amounts of organic matter and nutrients. Nutrient-rich lakes, called eutrophic lakes, usually are found at lower altitudes. Many plants and animal species are present as a result of organic matter and plentiful nutrients, some of which come from agricultural and urban activities.