TECTONIC GEOMORPHOLOGY Landslides limit mountain relief

被引：31
|
作者：
Roering, Josh [1 ]
机构：
[1] Univ Oregon, Dept Geol Sci, Eugene, OR 97403 USA
来源：
NATURE GEOSCIENCE | 2012年 / 5卷 / 07期
关键词：
ROCK UPLIFT; INCISION;
D O I：
10.1038/ngeo1511
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
Despite variable forcing by tectonics, the height of mountain ranges seems to be limited. Satellite imagery suggests that landsliding rates adjust to large changes in uplift, acting to maintain hillslopes of similar steepness.
引用
下载
收藏
页码：446 / 447
页数：2
相关论文
共 50 条
  • [1] Landslides limit mountain relief
    Josh Roering
    Nature Geoscience, 2012, 5 : 446 - 447
  • [2] High-mountain landslides in the Atlantic Pyrenees: their relationship with the geology and geomorphology
    T. Lebourg
    R. Fabre
    B. Clement
    M. Frappa
    Bulletin of Engineering Geology and the Environment, 2003, 62 (3) : 221 - 229
  • [3] Valles Marineris landslides: Evidence for a strength limit to Martian relief?
    Bigot-Cormier, Florence
    Montgomery, David R.
    EARTH AND PLANETARY SCIENCE LETTERS, 2007, 260 (1-2) : 179 - 186
  • [4] TECTONIC GEOMORPHOLOGY
    BULL, WB
    WALLACE, RE
    GEOLOGY, 1985, 13 (03) : 216 - 216
  • [5] TECTONIC GEOMORPHOLOGY
    BULL, WB
    JOURNAL OF GEOLOGICAL EDUCATION, 1984, 32 (05) : 310 - 324
  • [6] TECTONIC GEOMORPHOLOGY
    SUMMERFIELD, MA
    PROGRESS IN PHYSICAL GEOGRAPHY, 1991, 15 (02) : 193 - 205
  • [7] Mountain geomorphology
    Pain, Colin
    GEOGRAPHICAL RESEARCH, 2007, 45 (03) : 320 - 321
  • [8] Mountain geomorphology
    Rea, BR
    GEOGRAPHICAL JOURNAL, 2006, 172 : 84 - 84
  • [9] Active Deformation and Relief Evolution in the Western Lurestan Region of the Zagros Mountain Belt: New Insights From Tectonic Geomorphology Analysis and Finite Element Modeling
    Basilici, Matteo
    Ascione, Alessandra
    Megna, Antonella
    Santini, Stefano
    Tavani, Stefano
    Valente, Ettore
    Mazzoli, Stefano
    TECTONICS, 2020, 39 (12)
  • [10] TECTONIC CAUSES OF LANDSLIDES
    ALEXANDER, D
    FORMICHI, R
    EARTH SURFACE PROCESSES AND LANDFORMS, 1993, 18 (04) : 311 - 338
12345