Add to ORKGHuangshan (Yellow Mountain) is located in southern part of the lower reaches of the Yangtze River. The highest Lotus Flower peak is 1,864 m above sea level. Formative ages of the Huangshan and its granite, process of mountain geomorphic evolution from the Eocene to Quaternary, environmental changes of Quaternary, formative origin of beautiful peaks and fascinating rocks were studied and the questionable “Pleistocene glaciation” was also discussed in this paper
This paper deals with the study of Holocene geomorphic evolution of rivers around Songshan Mountain ...
This paper deals with the study of Holocene geomorphic evolution of rivers around Songshan Mountain ...
This paper deals with the study of Holocene geomorphic evolution of rivers around Songshan Mountain ...
Huangshan (Yellow Mountain) is located in southern part of the lower reaches of the Yangtze River. T...
Huangshan (Yellow Mountain) is an 1864-m granite massif situated at 30 10 N and 118 11 E, south of t...
Huangshan (Yellow Mountain) is an 1864-m granite massif situated at 30 10 N and 118 11 E, south of t...
The upper–middle Yellow River flows through the Fenwei graben, a structure resulting from extensiona...
The various types of granite landforms in the Huangshan Mt. are distributed in a concentric pattern....
The various types of granite landforms in the Huangshan Mt. are distributed in a concentric pattern....
The Yellow River basin (YRB) has played an important role in the forming of Chinese civilization. Lo...
Both the Lushan and the Huangshan have been regarded as sites of Pleistocene glaciation since the pi...
Both the Lushan and the Huangshan have been regarded as sites of Pleistocene glaciation since the pi...
We present geomorphological evidence for multiple glacial fluctuations during the Quaternary in the ...
At about 173 ka BP of the late period of mid-Pleistocene, the second terrace of the river had been f...
Recently, the “mountain-geobiodiversity hypothesis” (MGH) was proposed as a key concept for explaini...
This paper deals with the study of Holocene geomorphic evolution of rivers around Songshan Mountain ...
This paper deals with the study of Holocene geomorphic evolution of rivers around Songshan Mountain ...
This paper deals with the study of Holocene geomorphic evolution of rivers around Songshan Mountain ...
Huangshan (Yellow Mountain) is located in southern part of the lower reaches of the Yangtze River. T...
Huangshan (Yellow Mountain) is an 1864-m granite massif situated at 30 10 N and 118 11 E, south of t...
Huangshan (Yellow Mountain) is an 1864-m granite massif situated at 30 10 N and 118 11 E, south of t...
The upper–middle Yellow River flows through the Fenwei graben, a structure resulting from extensiona...
The various types of granite landforms in the Huangshan Mt. are distributed in a concentric pattern....
The various types of granite landforms in the Huangshan Mt. are distributed in a concentric pattern....
The Yellow River basin (YRB) has played an important role in the forming of Chinese civilization. Lo...
Both the Lushan and the Huangshan have been regarded as sites of Pleistocene glaciation since the pi...
Both the Lushan and the Huangshan have been regarded as sites of Pleistocene glaciation since the pi...
We present geomorphological evidence for multiple glacial fluctuations during the Quaternary in the ...
At about 173 ka BP of the late period of mid-Pleistocene, the second terrace of the river had been f...
Recently, the “mountain-geobiodiversity hypothesis” (MGH) was proposed as a key concept for explaini...
This paper deals with the study of Holocene geomorphic evolution of rivers around Songshan Mountain ...
This paper deals with the study of Holocene geomorphic evolution of rivers around Songshan Mountain ...
This paper deals with the study of Holocene geomorphic evolution of rivers around Songshan Mountain ...