气候的周期性变化使河流发生周期性的堆积与侵蚀，会形成一系列阶地。
Periodic climate changes cause periodic river accumulation and erosion, resulting in a series of benches.
构造运动和气候变化是制约内陆地区河流阶地发育的两个关键因素，而不同地区的河流对它们的响应方式多种多样。
Tectonic uplift and climate change are two key factors in controlling the development of river terraces in hinterlands.
由于河流阶地是间歇性新构造抬升的产物，其形成阶段又与气候的冷暖变化相关，即冷期阶地陡坎形成，暖期阶地堆积物形成。
Because the river terrace is the result of interrupting neotectonic uplift and its forming stages are bound up with the geologic climate cold warm changes, I.
由于河流阶地是间歇性新构造抬升的产物，其形成阶段又与气候的冷暖变化相关，即冷期阶地陡坎形成，暖期阶地堆积物形成。
Because the river terrace is the result of interrupting neotectonic uplift and its forming stages are bound up with the geologic climate cold warm changes, I.
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