Shi Men Jian Glacial U-Valley was formed about 100,000-900,000 years ago and is spaced by a series of ....
Shi Men Jian Valley is a box-shaped valley. It is far deeper than it is wide. It was formed along ....
Guan Ying Ge boulder clay was rediscovered when road workers cut through a part of hill. It was formed ....
A sheath structure is a conical form of rock that has been subjected to stretching and folding by ....
This is the most magnificent and steepest precipice in Lushan. The cliff is 700m long and is a group of ....
Jiu Die Valley Rheological Folds are located on the upper level of a metamorphic rock detachment fault. ....
Three Cascades Waterfall is located at the junction of Qing Lian and Jiu Die U- Valleys. It is 120m high. ....
Jing Qi Peak is a steep sandstone peak. It has been compared to a fluttering flag. Crust shearing created ....
Wu Lao Peak is a sandstone peak formed in the Nanhua Period (0.8 – 0.68 billion years ago). The sandstone ....
This firn basin was named by Li Si Guang, a famous geologist and the originator of geo-mechanics in ....
Han Po Lin is a ridge, shaped like a knife, formed by ice erosion. The ridge runs along the mountain in a ....
Tai Yi and Li Tou Jian peaks are glacial horns, pyramid-shaped peaks formed by glacial erosion. Tai Yi ....
The north part of Lushan is made up of sandstone. Shear joints developed within crevices, breaking off ....
The boulder clay profile is a fragmental deposit of debris carried down and deposited by glaciers. It is ....
This 1600m long U-Valley was caused by glacial erosion 0.9 -1.1million years ago. Water erosion and ....
The front of Lion Mouth Cliff looks like a lion’s mouth. It was formed by sandstone collapsing along ....
Tian Qiao Glacial Spillway is located in-between Xi Gu and Jin Xiu Gu glacial U- Valleys. The glacier ....
Ru Qin Lake is a firn basin, a place where glacial ice accumulates. When the climate changed, the basin ....
A glacial table refers to a slate of rock that is carried down from a higher level of the mountain by ....
A Quaternary glacier is a moving glacier created by accumulated snow. The glacial period started 3 ....
Lian Gu Hanging Valley is a valley that hangs above Wang Jia Po U- Valley. They are connected by a ....
В ущелье Шимен, имевшем форму буквы «U», в далёком прошлом находилась заполненная льдом впадина, которая ....
Ущелье Шимен образовалось за счет сил растяжения, в результате действия которых скальный грунт вышел на ....
Вершина Тысячи Будды – это горный пласт, который еще не полностью подвергся охлаждению и сдвижению, с ....
Острые края горной складки называют «зигзагообразными складками». Два крыла такой складки представляют ....
Скала «Битва Дракона с Тигром» сформировалась в результате реологии двух кварцевых жил. Кварцевые жилы ....
В период от 100 до 900 тысяч лет тому назад ледник, находившийся в долине Шимен, имел форму буквы «U». Он ....
Ущелье Шимен представляет собой вертикальный каньон, глубина которого значительно больше, чем ширина. ....
Der rote Boden hat sich vor drei Millionen Jahren gebildet. In der quartären Eiszeit war der rote Boden ....
Wenn sich das Klima erwärmt, ziehen sich die Gletscher zurück. Und wenn es kalt wird, bewegten sich die ....