A ridge is a long, narrow, elevated geomorphologic landform, structural feature, or a combination of both separated from the surrounding terrain by steep sides. The sides of a ridge slope away from a narrow top, the crest or ridgecrest, with the terrain dropping down on either side. The crest, if narrow, is also called a ridgeline. Limitations on the dimensions of a ridge are lacking. Its height above the surrounding terrain can vary from less than a meter to hundreds of meters. A ridge can be either depositional, erosional, tectonic, or a combination of these in origin and can consist of either bedrock, loose sediment, lava, or ice depending on its origin. A ridge can occur as either an isolated, independent feature or part of a larger geomorphological and/or structural feature. Frequently, a ridge can be further subdivided into smaller geomorphic or structural elements.
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👉 Hill ridge in the context of Hill chain
A hill chain, sometimes also hill ridge, is an elongated line of hills that usually includes a succession of more or less prominent hilltops, domed summits or kuppen, hill ridges and saddles and which, together with its associated lateral ridges and branches, may form a complex topographic structure. It may occur within a hill range, within an area of low rolling hill country or on a plain. It may link two or more otherwise distinct hill ranges. The transition from a hill chain to a mountain chain is blurred and depends on regional definitions of a hill or mountain. For example, in the UK and Ireland a mountain must officially be 600 m (2,000 ft) or higher, whereas in North America mountains are often (unofficially) taken as being 1,000 ft (300 m) high or more.
The chain-like arrangement of hills in a chain is a consequence of their collective formation by mountain building forces or ice age earth movements. Hill chains generally have a uniform geological age, but may comprise several types of rock or sediment.
Hill ridge in the context of Battert
The Battert is a hill, 567.9 m above sea level (NHN), on the western edge of the Northern Black Forest north of Baden-Baden in Germany. On its western slopes are the ruins of Hohenbaden Castle (the Altes Schloss or "Old Castle"), on the southern side is the climbing area and nature reserve called the Battert Rocks (Battertfelsen). On the hill ridge are the remains of a circular rampart, probably built by Celtic settlers. On the eastern side lies the village of Ebersteinburg.
The Battert is a destination for ramblers and climbers all year round, heading for the 15–60-metre-high Battertfelsen. Above and below the rock face is a footpath around the rocks. The red rock face is visible from far off and may be easily reached on the road to the ruins of Hohenbaden or from a car park near Ebersteinburg.
Hill ridge in the context of Stromberg (landscape)
The Stromberg (German pronunciation: [ˈʃtʁoːmˌbɛʁk] ) is a heavily forested hill ridge up to 476.6 m above sea level (NN) in the northern part of the German state of Baden-Württemberg.