Dongguang county scenic spot

The scenic spots in Dongguang County include Dongguang Tiefo Temple, Ma Zhiyuan Memorial Hall, Erlanggang Yongqing Temple, Dongguang Yuanqu Cultural Park and Hegou S

The scenic spots in Dongguang County include Dongguang Tiefo Temple, Ma Zhiyuan Memorial Hall, Erlanggang Yongqing Temple, Dongguang Yuanqu Cultural Park and Hegou Site. Dongguang County is located in the south of Hebei Province in North China Plain, in the lower reaches of Heilonggang River Basin and in the south of Cangzhou City.

South of wuqiao county, the two counties are 32 kilometers apart; Nanpi County is in the north, and the two counties are 20 kilometers apart; The west is bounded by the canal south of Fucheng County, and the two counties are 33 kilometers apart; The southwest is bordered by Jingxian County; Bordering Botou City in the northwest; East of Zhang Weixin River, facing Ningjin County.

Dongguang County has a flat terrain, gentle slope, high in the southwest and low in the northeast, with an altitude of 14.5~9 meters and a wave drop of110000 ~112000, which is mainly composed of gentle hills, depressions, two slopes and sand dunes.

Dongguang County has a warm temperate and semi-warm continental monsoon climate. Terrain has little influence on climate, and the general climate features are: distinct seasons, abundant sunshine, moderate temperature, and simultaneous rain and heat. The distribution of annual precipitation is uneven, which has the characteristics of spring drought, summer waterlogging and autumn hanging. Disastrous weather such as drought, flood, wind and hail, continuous rain and cold wave occur frequently.

The geotectonic structure of Dongguang County belongs to the North China Platform, which uplifted into land in the Middle and Late Paleozoic. The geological structure is located in the NE-trending fault structure of Xinhua Xia since the Miocene and belongs to Huanghua Depression in the subsidence zone of North China. As far as local structure is concerned, it is located between Cangxian uplift and Chengning uplift.

Generally speaking, Sinian and Paleozoic strata are developed and thick. The thickness of Eogene is very small, and the whole county is covered by extremely thick Quaternary strata, with no outcrop.