moutonnee
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The distributive laws of roche moutonnee and whaleback form is controled by icetemperature and dynamic process at glacial bottom.
羊背石和鲸背岩的分布规律是受底部冰温和动力过程控制的。
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In addition, the specific position of roche moutonnee is related with the local climate, structure and relationship between the primary trough and tributaory trough.
此外,羊背石分布的具体地点还与局部气候、构造以及主支谷之间的关系相关。
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According to the uplift rate of 0.133-0.4 cm/a, the old moraine was formed in 610±50 ka, the glacial rock surface was formed in 140±9 ka and the roche moutonnee was formed in 18.6±0.2 ka.
由于终碛垄是冰盛期结束时遗留下来的,而冰川擦痕面是冰期结束过程中暴露出来的,因此不同冰川地貌面反映的冰期中的冰川事件是不同的。
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On the contrary, some positions of roche moutonnee are not at the pressure-melt point, and the temperature of ice-base has cold and temperate alternately. They belong to the pluck-abrasion zone.
形成羊背石的部位与之相反,一些地方没有达到压力融点,冰底温度有冷、温的变替,是拔蚀-磨蚀作用带。
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According to the idea of uplift early, it can be calculated that the old moraine was formed in 459.42 ka BP, the glacial rock surface was formed in 122.5 ka BP and the roche moutonnee was formed in 18.3 ka BP.
根据80万年来的阶段性的隆升速率介于0.133 cm/a – 0.4 cm/a之间,计算出老终碛垄的形成年代为564.96 ka-656.27 ka,取值为610±50 ka;冰蚀基岩面的形成年代为130.85 ka-149.37 ka,取值为140±9 ka;羊背石的形成年代为18.494 ka-18.790 ka,取值为18.6±0.2 ka。
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- 更多网络解释与moutonnee相关的网络解释 [注:此内容来源于网络,仅供参考]
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moutonnee hummock:圆冰丘
Mouths of Rivers 河口 | moutonnee hummock 圆冰丘 | movable appendage 活动附体
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moutonnee:羊背石
山谷风 mountain-valley breezes | 羊背石 moutonnee | 可移动细网格模式 movable fine-mesh model (MFM)
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roche moutonnee:羊背石
rocha 岩石 | roche moutonnee 羊背石 | roche 岩石