复合火山形态测量中侵蚀的作用

R. M. M. van Wees, Pierre-Yves Tournigand, D. O’Hara, P. Grosse, G. Kereszturi, Benjamin Campforts, P. Lahitte, M. Kervyn
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引用次数: 2

摘要

火山是极具活力的地貌。它们因喷发产物和侵入物的积累而生长,并因一系列侵蚀过程而退化,如地表径流、化学和物理风化、河流和冰川切割以及大块运动。在这项研究中,我们的目标是使用一系列形态计量指标来记录和量化天然复合火山的形态,以更好地了解控制侵蚀速率和模式的因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The role of erosion in the morphometry of composite volcanoes
Volcanoes are extremely dynamic landforms. They grow by the accumulation of eruptive products and intrusions and degrade by a range of erosion processes such as superficial runoff, chemical and physical weathering, fluvial and glacial incision, and mass movements. In this study, we aim at documenting and quantifying the morphology of natural composite volcanoes using a range of morphometric indices, to better understand the factors that control erosion rates and patterns.
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