用英語(yǔ)說(shuō)中國(guó)旅游華東地區(qū)01：黃山自然概況2

特別提醒

Mt. Huangshan is geologically that of fully developed granite，with faults and cracks interlacing each other to form various amazing caves and crevices. Located in the zone of subtropical monsoon，the temperature drop as the altitude increases. Meanwhile，there is a sharp difference between the amount of sunshine，and the local terrain is the dominating factor of the local weather，name1y the distinctive mountain monsoon climate:foggy，humid，and rainy. The vertical zonality of the soils is obvious:yellow mountain soil below 900m above sea level， yellow brown soil at the altitude from 900m一1 600 m，and alpine meadow soil at the flat tops 1600m一1 840m above sea level.

黃山山體的花崗巖體發(fā)育完整，斷裂和裂隙縱橫交錯(cuò)，形成瑰麗多姿的洞穴、孔道。黃山處于亞熱帶季風(fēng)氣候區(qū)內(nèi)，山高吞深，氣溫垂直遞減。同時(shí)，北坡和南坡受陽(yáng)光的輻射差大，局部地形對(duì)其氣候起主導(dǎo)作用。形成了特殊的山區(qū)季風(fēng)小氣候—一云霧多、濕度大、降水多。黃山土壤的垂直分布地帶特性明顯，海拔900米以下為山地黃壤,900一1 600米為山地黃棕壤,1 600一1 840米為山頂平臺(tái)地域的高山草甸土。