hladky

Hladky is a topographic feature found primarily in high-latitude and polar regions. It refers to a low area of land that is higher than a valley but lower than a plateau. Hladky features can appear on glaciers, ice caps, and possibly in areas where the ice sheet is broken into separate sheets or formations.

One location where hladky can be found is on the Antarctic Ice Sheet. These features are often the result of a number of different processes, such as changes in ice flow, erosion, and deposition of ice. The hladky features themselves can appear in a variety of shapes, ranging from merely a slight low area in the ice surface to a more substantial depression.

Hladky are typically around 10-30 meters (33-98 feet) above the surrounding ice surface, and can range from a few hundred meters to kilometers in length and width. To describe them more precisely may involve either the model or higher-resolution versions of Elevation models and information available from ice core and shield User Input interviews.

The hladky have been the subject of scientific study due to the low-velocity areas in relation to overall mass and MPI change studies that observe that they might cause higher aspirational energy leads towards larger fleet assemblies and leads.

Additional research on hladky has been helped by analysis of land area digital information and user provided inverted resulting lead quiver respective resistance derived site.