MAIN FORMS OF TERRAIN RELIEF

Mualliflar

  • Otabek Abdisamatov Tashkent International University of Financial Management and Technologies, Senior Lecturer, Department of Architecture and Digital Technologies Muallif
  • Zohid Najimov Tashkent International University of Financial Management and Technologies, Department of Architecture and Digital Technologies, 2nd year student, Department of Geodesy, Cartography and Cadastre Muallif

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Terrain relief; landforms; geomorphology; macro-relief; meso-relief; micro-relief; hypsometry; slope analysis; tectonics; erosion.

Abstrak

Terrain relief—the spatial configuration of Earth’s solid surface—constitutes the fundamental template upon which climatic, biotic and anthropogenic processes play out. Although a bewildering variety of landforms exist, they can be organised into a hierarchy of main relief forms shaped by plate tectonics, weathering, erosion and deposition. This paper synthesises geomorphological theory and empirical data to identify the dominant morphographic units at three nested scales—macro-relief (continents, mountain belts, basins), meso-relief (hills, plains, plateaus, valleys) and micro-relief (ridges, gullies, dunes, yardangs). A meta-analysis of 112 peer-reviewed studies provides quantitative ranges for slope, hypsometry and process dominance within each unit.

Iqtiboslar

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Nashr qilingan

2025-05-26

Iqtibos keltirish tartibi

MAIN FORMS OF TERRAIN RELIEF. (2025). Yangi O‘zbekiston Pedagoglari Axborotnomasi, 3(5), 75-79. https://in-academy.uz/index.php/YOPA/article/view/26664