The Norwegian trench or Norwegian channel (Norwegian: Norskerenna; Danish: Norskerenden) is an elongated depression in the sea floor (but not a true oceanic trench) off the southern coast of Norway. It reaches from the Stad peninsula in Sogn og Fjordane in the northwest to the Oslofjord in the southeast. The trench is between 50 and 95 kilometers wide and up to 700 meters deep. Off the Rogaland coast it is 250 - 300 meters deep, and its deepest point is off Arendal where it reaches 700 meters deep – an abyss compared to the average depth of the North Sea, which is about 100 meters.

It was formed during the last 1.1 Ma by the effects of erosion associated with repeated ice stream activity The trench is not a subduction-related oceanic trench, where one tectonic plate is being forced under another. The Norwegian Trench was created by fluvial erosion processes during the later Tertiary age. Pleistocene glaciers and ice-sheets further deepened the trench. During the main glaciations, the Skagerrak Trough was the meeting point for ice from southeastern Norway, southern Sweden and parts of the Baltic causing a relatively fast-moving ice stream that passed south of the Norwegian coast and then turned north, eventually reaching deepwater at about 62°N. The material carried by the ice stream was then deposited in the North Sea fan. Glacial erratics such as flint and rhomb porphyry, thought to originate from the Skagerrak and Oslo areas respectively , and deformed glacial tills found on the coast of Jæren provide the main onshore evidence for the Norwegian Channel Ice Stream.