Which city does Laiyang City in Hunan belong to?

There is no Laiyang City in Hunan Province, but a county-level city in Yantai City, Shandong Province, which is known as "Pear Town". 1987, Laiyang was one of the earliest coastal cities in China. Laiyang City is located in the hinterland of Jiaodong Peninsula.

Laiyang, whose name comes from "Sun and Moon Rising to the East". In ancient times, it was called "Changyang" and "Changguang", also known as "Pear City" and "Dragon City".

Laiyang is located in the east of Shandong, bordering Yantai in the north and Qingdao in the south. It has been the "hinterland of Jiaodong" since ancient times. This is a hilly area with gentle hills and ravines. It belongs to temperate monsoon climate; It governs 5 streets, 13 towns, with a total area of 1734 square kilometers. In 20 17, the total population of Laiyang city was 880,000.

Laiyang is a specialty of Laiyang pear because of its unique climate and soil conditions, and is known as "Pear Town of China". The first dinosaur fossil in New China was found here, which is known as "the hometown of dinosaurs in China".

Laiyang has been called "the hometown of calligraphy" and "the hometown of calligraphy" since ancient times, and a number of patriotic literati have emerged. Laiyang is the birthplace of Quanzhen religion, known as the "ancestral home of Taoism", where Qiu Chuji and Ma Danyang once preached and founded schools. Laiyang is the birthplace of the national intangible cultural heritage "Mantis Boxing".

Laiyang has many tourist attractions with local cultural characteristics, such as Cretaceous National Geopark, Zhuocun, Li Xiang-style tourist area, Luer Port, Niangniang Mountain, Longwang Temple and Jinshan Tower.

References:

Laiyang city belongs to hilly area, with gentle hills and ravines. Due to the influence of Jiaodong back terrain, the terrain is inclined from north to south. There are unconnected low hills in the north, east, middle, southeast and southwest, which belong to the landform type of low hills.

Between rivers and mountains, valley plains and mountain basin plains are formed. Mountains account for 2 1.5% of the total area, hills account for 47.06% and plains account for 3 1.43%. The hilly area is distributed around the low mountain and its extension line, with an altitude of100 ~ 300m.

Its shale and volcanic rocks, the top of which is round, the slope of the hillside is generally between 5 ~15, the cross section of the gully is U-shaped, the longitudinal slope at the bottom of the gully is gentle, and the slope deposits are developed, and some of them are 5 ~ 8 meters thick.

The denudation and accumulation landforms of China plain and depression can be divided into three types of plains according to their causes. One is quasi-plain, which is distributed in bathhouse, Bailinzhuang, north of wulong village fault (except Laiyang basin) and south of Dakuang to Tuanwang. Most of them are distributed in the front of the hills in a strip shape; Second, the alluvial plain of intermountain valley is distributed in a strip shape on both sides of Wulong River;

Thirdly, the alluvial plain of intermountain basin, also known as depression, is distributed between Laiyang North Fault and wulong village Fault.

References:

Baidu Encyclopedia-Laiyang