többlyuk

Többlyuk, also known as "multihole" or "multi-hole" in English, is a term used in the field of geology and hydrology to describe a geological feature characterized by multiple interconnected or separate openings or cavities within a rock formation. These openings can vary in size and shape, ranging from small fissures to large chambers. The term is often used to describe features such as lava tubes, karstic caves, and other subterranean formations.

The formation of többlyuk structures is influenced by various geological processes. In volcanic regions, lava tubes are created when the outer layer of a lava flow cools and solidifies, while the molten lava beneath continues to flow, eventually leaving a hollow tube once the flow stops. In karstic regions, többlyuk formations can result from the dissolution of soluble rocks, such as limestone, by water, leading to the development of interconnected cavities and passages.

Többlyuk structures are of significant interest to geologists, speleologists, and other scientists due to their unique geological characteristics and potential for hosting diverse ecosystems. They can also have practical applications, such as providing habitats for various species, influencing groundwater flow patterns, and serving as potential sites for archaeological or paleontological discoveries. The study of többlyuk formations contributes to our understanding of geological processes and the evolution of landscapes over time.