Fjordähnliche
Fjordähnliche describes geological formations that resemble fjords but are not true fjords. True fjords are long, narrow inlets with steep sides or cliffs, created by glacial erosion and subsequently flooded by the sea. Fjordähnliche features share some of these characteristics, such as a U-shaped cross-section and steep valley walls, but their formation or inundation may differ.
These formations can arise from various geological processes. They might be river valleys that have been deepened
The term "fjordähnliche" is often used in geological and geographical contexts to differentiate these features from