Borebords
Borebords are a type of geological formation characterized by a series of parallel, elongated depressions or troughs that run across a landscape. These features are typically found in areas with specific geological histories, often related to glacial erosion or the movement of large ice sheets. The term "borebord" is derived from the Norwegian word "borebord," which translates to "ploughing board," reflecting the resemblance of these formations to the marks left by a plough.
The formation of borebords is thought to occur when glaciers move over soft, underlying bedrock. The immense
Borebords can vary significantly in size, from a few meters to several kilometers in length and from