黄河的发源地在青海的巴颜喀拉山上。

The source of the Yellow River can be traced to the Bayankela Mountains of Qinghai Province.

巴颜喀拉山脉南端位于四川省阿坝县、壤塘县与马尔康县交界地区。

The southern end of the Mts. Bayan Har lies in common boundary area of Aba, Zamtang and Barkam counties.

巴颜喀拉山北麓古高位湖相沉积的形成时代可能为中更新世。

The forming age of the lacustrine sedimentation from ancient high level lake at the north foot of Mt. Bayankala could be middle Pleistocene epoch.

重建的地层层序和沉积地质特征显示巴颜喀拉盆地主体三叠系复理石沉积是周缘前陆盆地。

The stratigraphic sequences and sedimentological characteristics indicate that the main body of Bayan Har Basin is composed of Triassic flysch sediments deposited in a foreland basin during Triassic.

喀拉喀托之子——阿那喀拉喀托在较为温和的喷发中稳定成长。

Anak Krakatau (' Child of Krakatau ') has been growing steadily through milder eruptions.