Water gap

A water gap is usually an indication of a river that is older than the current topography. The likely occurrence is that a river established its course when the landform was at a low elevation, or by a rift in a portion of the crust of the earth having a very low stream gradient and a thick layer of unconsolidated sediment.

In a hypothetical example, a river would have established its channel without regard for the deeper layers of rock. A later period of uplift would cause increased erosion along the riverbed, exposing the underlying rock layers. As the uplift continued, the river, being large enough, would continue to erode the rising land, cutting through ridges as they formed.

Water gaps are common in the Ridge-and-Valley Appalachians of eastern North America.

Alternatively, a water gap may be formed through headward erosion of two streams on opposite sides of a ridge, ultimately resulting in the capture of one stream by the other.

• Chicago Portage, Illinois - Saddle Point runs through the city itself.
• Columbia River Gorge, Oregon and Washington, and Wallula Gap, Washington, United States
• Cumberland Narrows, Maryland, United States
• Delaware Water Gap, New Jersey and Pennsylvania, United States
• Digby Gut, Nova Scotia, through which the Annapolis River flows into the Bay of Fundy
• Heavitree Gap, Alice Springs, Australia
• Iron Gates on the Danube River, forming the border between Serbia and Romania
• Kali Gandaki Gorge - cuts through the world's tallest mountain range, the Himalayas in Nepal
• Manawatu Gorge, New Zealand
• Middle Rhine in Germany
• Pongo de Mainique, Peru - on the Urubamba River
• Pongo de Manseriche, Peru - on the Marañón River
• Potomac Water Gap, United States
• Weltenburg Narrows on the Danube River in Bavaria
• Wawa Gorge, Rodriguez, Rizal, Philippines