澳大利亚中北部的一条长，2'公里(700英里)的间歇性河流，位于辛普森沙漠中。
An intermittent river, about, 2 'km (700 mi) long, of the Simpson Desert in north-central Australia.
澳大利亚中北部的一条长1,126公里(700英里)的间歇性河流，位于辛普森沙漠中。
An intermittent river, about 1,126 km (700 mi) long, of the Simpson Desert in north-central Australia.
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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