How do lakes end?

Exorheic, or open lakes drain into a river, or other body of water that ultimately drains into the ocean. Endorheic basins fall into the category of endorheic or closed lakes, wherein waters do not drain into the ocean, but are reduced by evaporation, and/or drain into the ground.



Lakes are transient geological features that "end" through two primary natural processes: infilling and drainage. Over thousands of years, rivers and streams carrying sediment, organic matter, and minerals deposit these materials into the lake basin. As this sediment accumulates, the lake becomes shallower, eventually transforming into a wetland, marsh, or meadow in a process called terrestrialization. Eutrophication can accelerate this, as excessive nutrients lead to algae blooms that die and settle on the bottom, further raising the basin floor. Alternatively, a lake can end through catastrophic or gradual drainage; this occurs when the natural dam holding the water back—such as a glacial moraine or a rock lip—erodes away or is breached by tectonic activity. Climate change also plays a significant role in 2026, as increased evaporation rates and diverted water sources cause many endorheic lakes to dry up completely, leaving behind salt flats or arid basins.

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The Life Cycle of Lakes All lakes, even the largest, slowly disappear as their basins fill with sediment and plant material. The natural aging of a lake happens very slowly, over the course of hundreds and even thousands of years. But with human influence, it can take only decades. A lake's plants and algae slowly die.

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The middle layer, the thermocline, mixes and turns over throughout the year. It turns over due to climate, nutrient variations, and geologic activity such as earthquakes. However, major lake turnover happens during the fall and spring, when the lake's cold and warm waters mix and readjust.

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Most of the world's millions of lakes are less than 18,000 years old and were formed when glaciers melted at the end of the last Ice Age. Geologists classify just 30 lakes, including Ohrid and Prespa, as “ancient”—defined by some researchers as persisting more than one ice age cycle (at least 130,000 years).

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Exorheic, or open lakes drain into a river, or other body of water that ultimately drains into the ocean. Endorheic basins fall into the category of endorheic or closed lakes, wherein waters do not drain into the ocean, but are reduced by evaporation, and/or drain into the ground.

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It may surprise you to know there is no technical difference between lakes and ponds, according to the National Park Service(Opens in a new window). However, a general rule of a thumb is if a body of water is large and deep it's a lake and if it's short and shallow it's a pond.

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Most lakes have at least one natural outflow in the form of a river or stream, which maintain a lake's average level by allowing the drainage of excess water. Some lakes do not have a natural outflow and lose water solely by evaporation or underground seepage, or both.

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Because warm water sinks in very cold freshwater, fish in these water bodies often gather in groups near the bottom. Some species, like koi and gobies, may burrow into soft sediments and go dormant like frogs and other amphibians, but most fish simply school in the deepest pools and take a winter rest.

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Turnover is like being at the mall … or at a fair. Turnover is a natural way the lake cleans up harmful bacteria and algae. It carries dead algae down into the depths of the lake where there is less sunlight, helping to prevent algae growth.

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