lapiés, weathered limestone surface found in karst regions and consisting of etched, fluted, and pitted rock pinnacles separated by deep grooves. This rugged surface is formed by the solution of rock along joints and areas of greater solubility by water containing carbonic and humic acids.

Lapies are a type of erosional landform formed in areas where the process of groundwater erosion is active. They are characterized by the formation of deep, parallel grooves or channels on the surface of rocks, particularly limestone, due to the dissolution of soluble materials by percolating water.

Lapies, also termed as Lapiaz, is a weathered limestone surface. When water flows over a surface having limestone along with other hard rocks, lapies are formed.

The meaning of LAPIES is grooves and ridges formed on a rock surface by solution of limestone.

May 5, 2022 · Lapies: Lapies are uneven grooves and ridges that form when the majority of the limestone's surface is removed by the solution process. Deep grooves separate the etched , fluted, and pitted rock pinnacles that make up the weathered limestone surface seen in …

Nov 16, 2021 · Lapies/ Karren. It is formed due to differential solution activity along parallel to sub-parallel joints. They are also called grooved, fluted and ridge-like features in an open limestone field. The most widespread surface karst landforms are small solution pits, grooves and runnels, collectively called Karren. Limestone Pavements

The term “lapiés” refers to a rill-like erosional form of limestone solution in the karst landscape. The term lapié is French, stemming from the type locality, Lapiaz. The term lapiésation was proposed for the process by Wray (1922).

Lapies correspond to those minor forms which in other terrains are the result primarily of mechanical denudation. In the roughness and inaccessi-bility of the terrain they are similar to the "bad lands" developed on clays and sands. But the formation of …

Question: What are lapies and how do they form? Answer: Lapies are irregular grooves and ridges on the surface of limestone bedrock, formed by the chemical weathering and dissolution of the rock by slightly acidic water.

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