Original text:

The people of the people have only received a glass of flowing wine, and I don't know when the flute and drums will be heard again today. The caves in Wuyi are full of poisonous bamboo, and those so-called great-grandchildren are old and will never come again.

Translation:

The villagers (called great-grandchildren) only got a glass of immortal wine from the immortals. I wonder when I will hear the sound of air flute and drum today. There are many poisonous bamboos growing in Wuyi Cave, and the villagers called great-grandchildren are old and never come again.

The author's character evaluation:

Poetry in the late Tang Dynasty tends to be worse than before, while Li Shangyin pushed Tang poetry to another peak. Du Mu was a famous poet in the late Tang Dynasty, and they were called "Little Du Li". Li Shangyin, Li He and Li Bai are collectively called "Li San" and Wen Tingyun is collectively called "Wen Li".

Brief introduction of Wuyishan:

Wuyi Mountain, also known as Hu Yi. Wuyi Mountain in a broad sense, or Wuyi Mountain Vein, refers to the mountain system running through the north and south between Fujian and Jiangxi in China, and belongs to the northeast extension branch of Nanling Mountain System, a new Cathaysian geological structural unit. In a narrow sense, Wuyishan only refers to the mountains in the main peak area under the jurisdiction of Wuyishan City in its northern section. It is a scenic spot of Wuyishan and a world cultural and natural heritage.

Geographical environment of Wuyi Mountain:

1, geology

Wuyishan vein is developed on Wuyishan uplift in Wuyishan fold belt. The axis of the northern part of the mountain is nearly east-west, and the southern part gradually turns to NE-NE; The middle section is northeast-northeast; The axial direction of the southern section is roughly north-south direction.

Wuyishan mountain range is mainly composed of upper Proterozoic schist, gneiss, granulite and migmatite. Sinian schist, gneiss, granulite, amphibole, quartzite and lenticular marble; Permian siltstone, sandstone, siliceous shale, shale and limestone.

2. Terrain

The two slopes in western Shandong are obviously asymmetrical, which is a remarkable feature of Wuyishan vein morphology. Due to the different crustal structures on both sides of the mountain, the ascending and descending movements are uneven. The slope of the eastern slope of Wuyishan facing Fujian is relatively gentle, and the ground is relatively uplifted, forming a series of mountains in the northeast-southwest direction, which gradually decreases from northwest to southeast in waves.

Step 3 plant

Wuyishan Mountain Range is a typical subtropical mountain range in China, with numerous peaks and severe topographic relief, forming a very complex and diverse combination of natural factors. Its flora belongs to the sub-zone of pan-Arctic flora and the sub-zone of East Asian forest flora, which is close to the northern margin of paleotropical flora.