Question 2: Is Tianjin Shell Dike Wetland Park good? It is the appropriate cusp of Oriental Technology, and it is the view of the other customers.
Question 3: Introduction of Tianjin shell dike Tianjin shell dike is one of the three famous ancient shell dikes in the world (the other two are Louisiana shell dike in the United States and Surinam shell dike in South America). It has been an important research object for scientists for decades, and occupies an important position in international research fields such as ocean, Quaternary geology, paleoclimate and paleoenvironment. It is a part of "Tianjin Ancient Coast and Wetland National Nature Reserve". The whole reserve is composed of shell dike, oyster beach and Qilihai wetland ecosystem, which is an extremely precious marine relic of ancient coastal changes. The research on shell dike, oyster beach and wetland in Tianjin has a history of several decades, and it has become an important place for marine, geology, geographical system and institutions to study coastal evolution, paleoclimate, wetland ecology and other disciplines.
Question 4: Where is the shell dike in Tianjin? How to get there? This is not a shell dike. The correct name is Dongtudi. Walk 3-5 minutes from Heping Road next to Bund Park to Haimen Bridge and Hebei Road. Take bus 1 10 or bus 6 17 (direction of Haimen Bridge).
Question 5: The composition of Tianjin shell dike The ancient shell dike in Tianjin, together with the shell dikes in Louisiana, USA and Suriname, South America, is called the three largest ancient shell dikes in the world, which plays an important role in the international Quaternary geological research. In the eastern part of Tianjin Plain, there are at least four shell dikes which are basically parallel to the modern coast. Shell dikes are distributed from north to south in Tianshuijing, Dasuzhuang and Shuyuanzi in Dagang District until Hebei Province. From 4500 to 4700 years ago, the shell dike was 22 ~ 27 kilometers away from the modern coast, and the shell species reflected the soft mud beach deposits in the inner bay of the coastal estuary. The nature reserve has established a sister reserve relationship with chesapeake bay National Estuary Research Reserve in the United States, and has been identified as a popular science education base in Tianjin.
Question 6: The formation of Tianjin shell dike The old Tianjin people called the ancient shell dike clam dike, which was deposited by the ancient shell dike and can reflect the changes of coastal land and sea. Tianjin ancient shell dike is one of the three largest ancient shell dikes in the world, which is of great significance to understand the geological evolution of Tianjin. As a special type of coastal dike, the ancient shell dike must have sediment, slope and hydrodynamic conditions suitable for shellfish breeding and being brought to the shore by heavy waves. Therefore, according to the location of the ancient shell dike, we can determine the location of the ancient coast, and according to the relationship between the old and new shell dikes, we can also analyze the evolution process and dynamics of the coast. Shell dike is a dike-like landform accumulation body which is composed of marine shells and their fragments and thin layers of fine sand, silt, peat and muddy clay, and is roughly parallel to the coast or has a small angle. It is formed near the * * * line of the sea and is a reliable symbol of the ancient coast in landform. Holocene transgression occurred from 5000 to 10000 years ago, which flooded most of Tianjin plain. After that, the sea level fell, rivers flooded and gradually became land. Shell dike is a relic left by this historical process, and it is a unique coastal landform type in Tianjin coastal zone, reflecting the change of coastline from land to sea. The dam is 0.5 to 5 meters high, tens to hundreds of meters wide and tens, hundreds or more than 100 kilometers long. There are many kinds of shells on the dike, mostly molluscs living in intertidal zone or shallow sea. Shellfish like to grow and breed on the fine sand and muddy seabed with clear and transparent seawater and rich nutrients. Under the action of waves, especially rough waves, shells and sediment will accumulate under the condition of suitable slope, and shell dikes will be formed near the * * * line. The Yellow River is a world-famous river with high sediment concentration, which has changed its course seven times. The natural conditions along the coast of Tianjin are favorable for the formation and development of shell dikes when Shandong is in the sea. However, when moving northward to Tianjin to enter the sea, the turbidity of seawater increases and the slope gradient slows down, and its ecological environment and dynamic conditions are not conducive to the formation of shell dikes. Therefore, the shell dike not only represents the coastline position in a certain period, but also reflects the geographical environment at that time. Since 1970' s, the formation period of shell dike has been studied by using carbon isotope absolute dating method and archaeological method. It is generally believed that the third dike was formed in Shang Dynasty about 3500 years ago. The second dam was formed during the Warring States period about 2000 years ago. Diyi appeared in the late Yuan Dynasty and early Ming Dynasty. From this, we can understand the development process of coastal land formation in Tianjin area.
Question 7: Where is the Beiti in Tianjin? Urgent, urgent, urgent! Three shell dikes have been discovered, which are distributed along the west coast of Bohai Bay from east to west.
Dike No.1 starts from Gaoshangbao in the north and joins Dike No.2 in the south via Caijiabao, Lvju River, Gaoshaling, Mapengkou to Qikou, with an altitude of 3-4 meters, mostly arc-shaped residual hills, and a dike is continuously formed from Mapengkou to Qikou.
The second dike is distributed in Baishaling, Junliangcheng, Gu Ni, Shanggulin, Qikou, Jiajiabao and Langtuozi, with a sea area of 3-4m. This series of dikes is continuous and basically complete.
The third dike passes through Xiaowangzhuang, Zhang Gui Zhuang, Jugezhuang, Shajingzi and Xiliuguanzhuang. 4~5 meters above sea level. Some areas are covered by late sediments and exposed near Jugezhuang, but the man-made damage is serious.
There are more than 0/0 species of shellfish/kloc-0 in the dike, such as Scapharca subcrenata, Meretrix meretrix, Ampullaria gigas, sole, soft-shelled turtle and so on. Shell dike is a kind of dike-like sediment composed of shell and its debris mixed with sand.
Question 8: Where are the interesting places in Tianjin seaside? One: Bertie.
1: Shell dike is a dike-like landform accumulation body composed of marine shells and their fragments, thin layers of fine sand, silt, peat and argillaceous clay, which is roughly parallel to the coast or has a small angle. Formed near the * * * line, it is a reliable sign of the ancient coast in landform. There are four shell dikes I, II, III and IV in Tianjin continental plain from the land to the sea, which are generally parallel to the modern coastline and distributed discontinuously in the form of ridges and hills, representing the position of the coast in four periods. /kloc-from 0/000 to 5,000 years ago, most areas of Tianjin Plain were submerged by transgression. After that, the sea level fell, rivers flooded and gradually became land.
2. Shell breakwater is a relic left by this historical process, a unique coastal landform type in Tianjin coastal zone and a relic of the ancient coast of Bohai Bay, which reflects the change of coastline from land to sea. There are many kinds of shells on the dike, mostly molluscs living in intertidal zone or shallow sea. The dam is 0.5 ~ 5 meters high, tens to hundreds of meters wide and tens, hundreds or more than 100 kilometers long. The top of its cross section is convex, and its wings are thinned into a point.
3. Transportation route: You can take Bus No.652 and Convenience No.61and get off at Laoshanggulin Station.
It is about 58km away from the North Square of Tianjin Railway Station, 1 hour by car.
Two: Tianjin seaside resort
1: Tianjin seaside tourist resort was built at 1989, located at the seaside of Luju River in Tanggu, far from the industrial zone. Because most of its services and amusement facilities are built on water, it has the reputation of "Venice of the East". Known as the "seaside hot spring", Tianjin seaside resort, also known as the bathing beach, is one of the largest artificial bathing beaches in China. A flush slide with three straight slides and two rotating slides, the largest in China, with a height of 15m. Elegant environment, clear water and blue sky, fresh air, away from pollution and noise.
2. Compared with Beidaihe, Qingdao, Dalian and other beaches, Tianjin Beach has its own uniqueness. Because the beach here is extremely gentle, the slope is only one thousandth, so the tidal range is very large. At high tide, the gentle beach forms a vast natural bathing beach with suitable water depth, and swimmers can swim in the distance of the sea. At low tide, a beach with a width of 2-3 kilometers is exposed, which is an ideal place to catch the sea. The bathing area is about180,000 square meters. An approach dike with a width of10m and a length of 600m has been built from the coast to the beach. An artificial beach with a width of 50 meters, a height of 5.5 meters and a length of 520 meters parallel to the coast is connected to the approach embankment. Visitors can enjoy picking up shells, catching fish, catching crabs and so on on the wide and flat beach.
3. Transportation route: It starts from the center of Tianjin, the whole journey is 54.9 kilometers, and it takes about 1 hour and 32 minutes to arrive.
Three: Tanggu Beitang Fishing Village
1: Beitang is located in the northernmost part of Tanggu District, Tianjin, bordering Bohai Bay in the east, Tianjin Port in the south, Development Zone in the west and Chemical Industry Park (Zone) in the north. Its natural environment is quiet and quiet, and it has been called "the hometown of Zeguo" since ancient times. In the early Qing Dynasty, it was already a famous fishing town in Tianjin and Yidong.
2.2 1 century, the tourism resources of Beitang have become increasingly prominent. Beitang seafood, Beitang Haihui, a day of fishing at sea, strong nostalgia, local customs and simple folk customs have all become the unique tourist landscape of Beitang. With rich historical and cultural connotations and the features of the triangle wetland nature reserve, it is a multifunctional tourist area integrating Haihe River sightseeing, fisherman's wharf, international cruise, seafood catering and customs culture.
Question 9: How far is the driving route from Tianjin shell dike to Cangzhou? The whole journey is about 162.4 km.
Starting point: shell dike wetland park
1. Tianjin city driving plan
1) Drive northeast from the starting point, follow the Central Avenue for 630m, and turn around and enter the Central Avenue.
2) Drive along Central Avenue for 6.0km, drive in the direction of S204/ Tang Han Road /S20/ Beijing-Tianjin Expressway, turn right slightly, and enter the Jishugang Bridge.
3) Drive along Jishugang Bridge for 2 10/0m, cross Central Avenue Bridge for about 220m, and go straight into Beijing-Tianjin Expressway.
4) Drive along the Beijing-Tianjin Expressway 14.8km, cross the overpass of Tanghuang Highway, turn slightly right in the direction of Tangshan/Huanghua /G25, and enter the North Ring Railway Overpass.
2. Drive along the North Ring Railway Overpass 1.0 km and go straight into expressway, Shen Chang.
3. Drive 54.9 kilometers along Shen Chang Expressway to Daqiuzhuang/Beijing/Economy /S60, turn left slightly and enter Shi Bin Expressway.
4. Drive 850 meters along Shi Bin Expressway, cross Tuanbo South Interchange and go straight into Shi Bin Expressway.
5. Drive 20.7km along Shi Bin Expressway, cross Wang Guan Tun Interchange, go to Cangzhou /S6, turn right slightly, and enter Wang Guan Tun Interchange.
6. Drive along Wang Guan Tun Interchange for 670 meters, cross Wang Guan Tun Interchange for about 320 meters, and go straight into Jincang Expressway.
7. Drive along Jincang Expressway 12. 1km, cross Zhangtun Interchange and go straight into Beijing-Shanghai Expressway.
8. Drive along the Beijing-Shanghai Expressway for 3 1.8km, turn right slightly in the direction of Cang Lang/Cangzhou/Fuyang Avenue/Huanghua Port, and enter the Beijing-Shanghai Expressway.
9. Drive along Beijing-Shanghai Expressway 1.6km and go straight into Cangzhou Ring Expressway.
10. Cangzhou driving plan
1) Drive along Cangzhou Ring Road for 3.6 kilometers, get off at Cangzhou/Fuyang Avenue exit, and turn right slightly on the ramp.
2) Drive along the ramp 1.4km and go straight.
3) Drive 4.7 kilometers and go straight into Fuyang North Street.
4) Drive along Fuyang North Avenue for 3.9 kilometers, pass Rongchang Mall on the left for about 70 meters, then turn left slightly and enter Fuyang South Avenue.
5) Drive 890 meters along Fuyang South Avenue, pass the left news building for about 90 meters, and enter Jiefang West Road.
6) Drive 420 meters along Jiefang West Road, turn right slightly and enter Jiefang West Road.
7) Drive along Jiefang West Road for 90 meters and reach the finish line.
End point: Cangzhou City
Question 10: Where is the shell dike? Shell dike is located in Jinnan, Dagang and Tanggu in the east of Tianjin. Shell dike is an ancient marine relic more than 7000 years ago. It is a dike-like landform accumulation body composed of marine shells and their fragments and thin layers of fine sand, silt, peat and muddy clay under the action of tides and wind waves.