Base level

The base level of a river or stream is the lowest point to which it can flow, often referred to as the 'mouth' of the river. For large rivers, sea level is usually the base level, but a large river or lake is likewise the base level for tributary streams. A rather rare exception can be seen in the Jordan River, for which the base level is the Dead Sea, 417 m below modern sea level.

When the source of a stream is very high, relative to the base level (high stream gradient), erosion proceeds rapidly due to the energy of the rapidly moving water; the topography becomes rugged; and we say the stream is young (geologicially speaking). When erosion has acted for a long geologic time, wearing down the high points and making a small difference between the source and the base level of a stream (low sream gradient), we say that it is mature. Mature stream valleys have gentle slopes, rounded higher points and meandering courses.

A very hard layer of rock can form a temporary base level, until it is cut through. The Lockport dolomite has created a temporary base level for the Niagara River. Eventually this will be cut through as Niagara Falls recedes, and Lake Erie will be drained to near the lower base level of Lake Ontario.

Movements of land can greatly affect base levels. The uplift of the Colorado Plateau, combined with the opening of the Gulf of California to the sea, established sea level as the base level for the Colorado River and led to the (geologically) rapid erosion that resulted in the Grand Canyon.

The many meaders of the Kentucky River shows that it was a mature stream with little relief. Uplift of the central Kentucky area rejuvinated the stream, causing it to cut a deep canyon, but preserving the meanders that indicate the stream existed prior to the uplift.

Other geologic processes can affect base levels. In the Finger Lakes of New York, Ice age glaciation greatly deepened the lake valleys and rejuvinated tributary streams. These streams have deep ravines and often waterfalls where hard rock layers slow erosion; they are said to be hanging valleys. A mature tributary stream has a greatly reduced stream gradient at it approaches the base level.

Sea level can also change (primarily due to the formation or melting of continental ice sheets), and raise or drop the final base level for coastal rivers. Along the east coast of North America river valleys extend out onto the continental shelf indicating a time when erosion was possible due to the lower base level of a lower sea level in the past. Today many of these same rivers end in bays, indicating that sea level has risen in recent geologic time. This is referred to as a drowned coastline.


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