Zhangqiu people have a long history of labor and business, and are known as the "hometown of blacksmiths". There are Baimaiquan, Baiyun Lake, Qixingtai, Jingping Natural Scenic Area, Chengziya Site, Dongping Mausoleum Old City, Qi Great Wall and other historical sites. The Han Tomb in Luo Zhuang and the Terracotta Warriors and Horses in Dangerous Mountain discovered in recent years are famous at home and abroad. Celebrities come forth in large numbers, which is the hometown of Zou Yan, a philosopher in the Warring States period, Fang, a famous figure in the Tang Dynasty, Li Qingzhao, a poet in the Song Dynasty, and a famous commercial capitalist in modern times. Rich in resources, there are 25 kinds of proven mineral resources, which are national key coal-producing counties (cities), high-quality bauxite export bases and limestone storage areas. Excellent geographical location, convenient transportation and strong industrial supporting capacity. Ji Jiao Railway, Qing Ji, Wang Ji Highway and Qing Ji Expressway run through the east and west, and 09 Road and Zhanglai Highway run through the north and south. Jinan International Airport is 35 kilometers away from Mingshui. With a solid industrial base, it has formed four major industries: transportation equipment, machinery manufacturing, fine chemicals and food and beverage. In 2008, the GDP was 37.4 billion yuan, and the local fiscal revenue was 2.003 billion yuan. It ranked 40th among the top 100 comprehensive strength of small and medium-sized cities in China in 2008, and won the top 100 with the most investment potential, the top 100 with the most regional driving force, and the top 100 economical small and medium-sized cities in China 10.
geographical position
Zhangqiu is located in the middle of Shandong Province, 50 kilometers east of Jinan, 70 kilometers north-south and 37 kilometers east-west, with a total area of 1855 square kilometers. Geomorphologically, Zhangqiu belongs to Luxi fault block area. The Telu block in the western Shandong fault block is uplifted, and the Paleozoic strata are exposed from new to old, and the oldest limestone in the middle and upper Cambrian is exposed, forming the southern community: sandstone shale in the middle and upper limestone of Devonian is exposed near Mingshui, and igneous rocks are mainly exposed near Changbai Mountain in the northern Xiaoba. The former is permeable and the latter is impermeable. In addition, the terrain is high in the south and low in the north, and the groundwater gathers from south to north. When the water head near Mingshui is blocked, it emerges from the ground and forms a spring group. Therefore, there are many springs and water in Mingshui.
climate
Zhangqiu belongs to the continental climate of warm temperate monsoon region, with four distinct seasons, rain and heat in the same season, drought and windy in spring, concentrated rainfall in summer, mild and cool in autumn and dry and cold in winter. The annual average sunshine is 2647.6 hours, the annual average temperature is 12.8℃, the annual average precipitation is 600.8 mm, the relative humidity is 65%, and the frost-free period is 192 days.
geology
The southern part belongs to Luxi uplift area, and the northern part belongs to Jiyang depression area, which belongs to the Luxi system of rotating structure.
In the stratosphere, north-south and northwest compressive and torsional faults are developed. Especially the Wen Zu fault, two plates in the north-south direction.
Moving 15km, the topography, geology and groundwater sources on both sides of the fault have formed obvious differences between the east and the west.
The geological structure is generally monoclinic strata, with massive faults and few folds. Strata strike is 60 degrees northwest.
30 to the northeast with an inclination of 7 ~ 13. The strata of every geological age are complete. The distribution of mountainous areas from south to north is as follows
Metamorphic rock, limestone, shale, coal seam, volcanic eruption rock, etc. Hilly valleys and alluvial plains are widely distributed.
Mudstone distribution, the lower part is fresh water limestone, and the upper part is gravel layer and various soils.
zone
Great Wall Ridge is located at the northern foot of Taiyi Mountain, bordering the North China Plain and Changbai Mountain in the south.
Standing in the east. The terrain slopes from southeast to northwest. From south to north, there are mountains, hills, plains and depressions in turn.
They account for 30.8%, 25.9%, 30.7% and 12.6% of the city's total area respectively. The highest peak is the chicken feet in the south.
Top, 924 meters above sea level; The lowest point is in Zhujiawa area of Xinzhai Township in the north, with an altitude of 15m.
The climate is in the middle latitude and belongs to the continental climate in the warm temperate monsoon region. Four distinct seasons, less rain and snow in winter and spring,
Rainfall is concentrated in summer. The average annual sunshine is 2647.6 hours; Annual average temperature 12.8℃, high temperature year 13.6℃, low temperature year.
Year11.7℃; The average annual precipitation is 600.8 mm, generally 500 ~ 700 mm. Monsoon, due to the terrain
The influence is not obvious, except for C (still wind) and SSW (south-southwest), which are the most wind directions in May.
He thinks C (still wind) and ESE (southeast east) are the dominant winds in January. Relative humidity 65%, frost-free period.
192 days.
hydrology
Most of the territory belongs to Xiaoqing River system, and a few mountainous areas in the southeast belong to Dawen River system. Master clock
Things are the Yellow River, Xiaoqing River, Jiangxiu River, Balou River, Luohe River and Juye River. The Yellow River is in the northwest.
Boundary River, from the southwest of Datan in Licheng District, enters zouping county at Changjiazhuang in Huanghe Township, with a flowing water of 27.08.
Km, with an average annual runoff of 42.5 billion cubic meters. Xiaoqing River is located in the northwest and comes from the northeast of Beichaijiazhuang in Licheng District.
Xiaojiazhuang of Shuizhai Town entered zouping county, with a transit reach of 18.8km and a drainage area of16,51.6km2.
The average annual runoff is 7.77 cubic meters per second. Xiuhe River, which originated from Mingshui Baimai Spring, is 32.8km long and injected.
Xiaoqing River. Dongbalou River, a seasonal river in the southeast, originated in Boshan District of Zibo City and entered through Shimen.
Xianggongzhuang Town stockade enters the Luohe River, with a total length of 34.4 kilometers. Xibalou River, located in the south-central, is a seasonal river with its source.
It is 68.8 kilometers long from the north slope of Sijiao Town to the north of Jinpan Village in Xiuhui Town. Luohe,
In Longwantou, Xianggongzhuang Town, it is connected with Dongbalu River and enters Nha Trang Lake in the northeast of Diaozhen Town, with a total length of 28 kilometers. Juye River,
The west branch originated from Bazhi Spring in Dalongtang, Licheng District, the east branch originated from the west of Beicaofan Village, and the two branches meet in the north of Longshan Town.
Zhangdu Reservoir, with a total length of 46.8 kilometers. The main lake is Baiyun Lake, located in the northwest, with a total area of 17.4 square kilometers.
The water area is 7.5 square kilometers and the water depth is 1 ~ 3 meters. Nha Trang Lake, in the northeast corner of the city, with a total area of 5.38 square meters.
Square kilometers, the water area is 2. 17 square kilometers, and the water depth is generally 1.9 meters.
What's the difference between a working doctor and a full-time doctor?
First, the enrollment methods are different.
On-the-job doctoral education is a