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The main body of Xinglongshan Nature Reserve is from Xinglongshan、Magnatal Mountain and Mountain Valley Composition。The location of the earth structure belongs to the southeast end of Qin Qi in the Qin Qi -Qin Qi between Qilian Mountain Trunlet Folding and Qinling，The secondary construction unit is Qingshi Ridge -Ma Tuoshan Folding Dome and Xinglong Mountain Caval with the Horses Mountain horizontal band。Former Zhendan and Zhendanpi，m88 best betting websiteThis area accepts a set of ground groove -shaped fragrance、Gravite、Mud rock、acidic and neutral volcanic debris rock、Macrobia and salt rocks such as medium base volcanic rocks and hydrochloride rocks。Lu Liang Movement of the former Zhen Dan Ji made it fold back，Forms the construct contour of the horseshill mountain backward and the back -to -back，and accompanied by different nature of fracture activities，It produced a strong mixed rockization in its later stage，All kinds of hybrid rocks in the wide -ranging horse titles are formed。Galidong Movement further suffers from regional deterioration in this area，Lile the constructive features of Xinglongshan Retevation Test。Relatively speaking，Yanshan Movement and Himalayan movement is not very strong in this area，On the contrary，New structure movement is more active，Make this area constantly rising。

The soil in the protected area is mainly gray -brown soil developed by stone mountains，In addition, there are also alpine meadow soil、Ya Gaoshan Caotou soil、chestnut calcium soil and new accumulation。No complete distribution belt，It is often due to the relationship between the slope becoming a zone soil region。

The slope of the Gorge is high due to the high terrain，Moving m88 reviewmore，low temperature，Steaming weakness，Large vegetation cover，The soil owner is gray -brown soil。Different from the terrain and slope，Causes changes in climate and plants，Different dilute gray -brown soil develops。The zone of the forest land of the slopes of the slopes is dilute gray -brown soil。Chengtu mother is a thousand rocks、Xuanwu Rock、Gart of sand、volcanic rocks and other residues、slope accumulation and loess substances, etc.。General fertility is higher，Organic mass content is 1.03-1.63%，But the soil layer is shallow。

Alpine meadow soil distribution includes 2 sub -categories of alpine meadow soil and alpine thyrted meadow soil，Corresponding to the mixed rocky meadow soil and mixed rocky alpine thymers 2 soils。distributed in a gentle mountain ridge and hillside in the protected area above 3500m，Deep soil layer，Chengtu mother is mainly based on the residual accumulation of mixed rock hemp rocks and mixed rocks。The area of ​​about 512hm2，accounting for 1.54%of the total area。

Asuka Mountain meadow soil includes 2 sub -categories in the Asuka Mountain Caudou soil and the Asuka Takayama Takamoto，Corresponding to carbonate rockyama meal meadow soil、Hybrid rocky mountain shy meadow soil and medium -based volcanic rocky mountain m88 live casino gamesshine meadow soil 3 soil。Distributed in the horse title between the 3000-3500m altitude of the protected area、The rising area of ​​Qianshan，Cheng Tu's mother quality with mixed tablets、Carbonate rocks and medium -based volcanic rock slopes are the main。Rich organic matter，Duan group granular structure，Calcium carbonate is scrubbing complete，SiO2 distribution evenly。A area of ​​about 4644hm2，accounting for 15.70%of the total area。

Gray -brown soil is the gray -brown forest soil，is the main Yilin soil of the protected area，It is mainly distributed in a forest belt between 2200-3000m altitude。Including the soluble gray brown soil、Gray -brown soil and lime -based gray -brown soil 3 sub -categories，Mixed rocky gray brown soil、Medium -based volcanic rock -soluble gray -brown soil、Carbonate spy -soluble gray -brown soil、Mixed rock gray -brown soil、Medium -based volcanic rock gray -brown soil、Carbonate gray -brown soil、Mixed rock lime gray -brown soil、Mid -found volcanic lime lime gray -brown soil、Carbonate lime -based gray -brown soil 9 soil。Chengtu Mother Qian Mountain with a deterioration Xuanwu Rock、Anshan Xuanwu Rock、Ninging Rock、Thousands of rocks such as the rocky airmade，Houshan is the slope accumulation of m88 live casino gamesvarious mixed rocks in the former Zhendan department。Gray -brown soil is from the withered layer、Exus quality layer、Correcting layer and the mother layer composition，Earth layer loose、Good structure，rich organic matter。A area of ​​about 21833hm2，accounting for 73.8%of the total area。

chestnut calcium soil only includes 1 sub -category of dark chestnut calcium soil，It is the soil developed under the vegetation of the dry grassland。Only sporadic distribution in the intertwined slope or Taiwan，Generally below 2100m，Delivery is small。Cheng Tu's mother is mainly the fourth discipline loess and white -crickets gravel，Clear soil，Duan granular structure，Strong organic mineralization，Weak humus accumulation。

The new accumulation is the recent flow of water、Soil formed by the formation of Hong accumulation，For the beginning of the soil，Short forming time，There is no obvious soil process，Basically maintained the maternal characteristics when deposited，Earthwriting，Lack of viscosity，龛。New accumulated soil is active in the reserve，Only see it in Xinglongxia、龛、Xiangshui ditch and other grooves，Postering the valley along the ditch，Fan -like distribution at the mouth of the ditch。

   Supply: Hao  Xin    Editor in charge: Zhang Yuanlin