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Liaodong Bay
Liaodong Bay () is largest and longest of the three main bays (along with Laizhou Bay to the south and the Bohai Bay to the southwest) of the Bohai Sea, the innermost gulf of the Yellow Sea. Although named after the Liaodong Peninsula (which forms its eastern shore), the bay is located directly south of the Liaoxi region, almost entirely west of the Liao River. It is bounded by the coastline of cities from southern Liaoning province (Dalian, Yingkou, Panjin, Jinzhou and Huludao) and eastern Hebei province (Qinhuangdao and Tangshan), between the Laotieshan Cape at Dalian's Lüshunkou District in the east, and the Daqing River estuary (which is an old southern mouth of Luan River) at Tangshan's Laoting County in the west. The major rivers that drain into the Liaodong Bay include Luan River, Daling River, Xiaoling River, Liao River and Daliao River. See also * Geography of China * Bijia Mountain Bijia Mountain () is an island located in the Liaodong Bay of China's Bohai Sea, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Huludao
Huludao (), formerly known as Jinxi () until 1994, is a coastal prefecture-level city in southwestern Liaoning province, People's Republic of China. Its name literally means "Gourd Island", referring to the fiddle-shaped contour of the peninsula ("half-island" in Chinese), which resembles a bottle gourd, at the city's Longgang District. It has a total area of and as of the 2020 census a population of 2,434,194 of whom 1,252,660 inhabitants lived in the built-up (or metro) area made of the 2 urban districts and Xingcheng City largely being conurbated. Located on the northwestern shore of the Liaodong Bay, Huludao is one of the three principal cities (along with Jinzhou and Hebei province's Qinhuangdao) in the Liaoxi Corridor, and is Northeast China's gateway through the Shanhai Pass into North China. It borders Jinzhou to the northeast, Chaoyang to the north, and Qinhuangdao to the southwest, as well as sharing maritime boundaries with Yingkou and Dalian to the east and s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bijia Mountain
Bijia Mountain () is an island located in the Liaodong Bay of China's Bohai Sea, south of the coast of the Jinzhou region of the Liaoning province, coastal China. During most times of the day, Bijiashan can only be accessed by boat. But when the sea recedes, a natural zigzagging cobblestone causeway (a tombolo), over 10 metres wide, links the island to the mainland. Location The island is located in the Jinzhou Economic and Technological Development Zone in Liaoning province, which is about 35 km from the city's downtown. It consists of the Bijia Mountain and the Celestial Bridge. Geography The mountain is a small island facing the Bohai Sea with its peak of 78.3 meter and a total area of 1.2 square kilometers. The name is derived from its unique penholder shape. The northern side of the mountain faces the mainland and is relatively flat with paved winding stone steps for tourists’ climbing, while the southern side is secluded and contains fewer visitors. It is fraught wi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of China
China has great physical diversity. The eastern plains and southern coasts of the country consist of fertile lowlands and foothills. They are the location of most of China's agricultural output and human population. The southern areas of the country (South of the Yangtze River) consist of hilly and mountainous terrain. The west and north of the country are dominated by sunken basins (such as the Gobi and the Taklamakan), rolling plateaus, and towering massifs. It contains part of the highest tableland on earth, the Tibetan Plateau, and has much lower agricultural potential and population. Traditionally, the Chinese population centered on the Chinese central plain and oriented itself toward its own enormous inland market, developing as an imperial power whose center lay in the middle and lower reaches of the Yellow River on the northern plains. More recently, the coastline has been used extensively for export-oriented trade, causing the coastal provinces to become the lead ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Daliao River
The Daliao River ( zh, s=大辽河, t=大遼河, p=Dàliáohé, "Great Liao River") is a major river system in eastern Liaoning province of Northeast China, and formerly the main distributary of the lower Liao River until 1958. The Daliao River ''proper'' is formed from the confluence of three rivers at the border between Anshan's Haicheng city and Panjin's Panshan County, after where it runs a length of covering a catchment area of , before coursing meandrously southwest and draining into the Liaodong Bay just west of Yingkou. The principal river of southern Northeast China, the Liao River, historically bifurcates into two distributaries near the Liujianfang Hydrological Station (六间房水文站) at Xinkaihe Town (新开河镇) of Anshan's Tai'an County, forming the Liao River Delta. The eastern distributary, called the Wailiao River, was originally the larger one and the main body of lower Liao River. It travelled southwards to pick up two large tributaries the Hun R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Daling River
The Daling River () is a river in Northeast China. With a length of , it is the main river in the arid western part of Liaoning. Its drainage basin covers , 85% of which is located in Liaoning, 13% in Inner Mongolia and the remaining 2% in Hebei. Course The Daling River has two sources. The southern source is Shuiquan Creek () in the village of Wukunzhangzi (吴坤杖子) in Jianchang County, Liaoning. The northern source is Quanzi Creek (泉子沟) in the village of Songyingzi (宋营子) in Pingquan, Hebei. The two source streams meet at Dachengzi, Kazuo County, Liaoning. From there the river flows northeast past the city of Chaoyang into Baishi Reservoir, where it receives Mangniu River (牤牛河) from the north. Baishi Reservoir is Liaoning's third largest reservoir with a capacity of . The reservoir was built on the Daling River between 1995 and 2001, primarily for flood control purposes, and secondarily to supply water to nearby urban and agricultural areas. At Baishi Res ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laoting County
Laoting County (), often mispronounced as Leting County in accordance with the alternative frequently used Mandarin pronunciation, is a county in the northeast of Hebei province, People's Republic of China, facing the Bohai Sea to the east and south. It is under the administration of Tangshan City. Geography and climate Laoting has a monsoon-influenced humid continental climate (Köppen ''Dwa''), with four distinct seasons and some maritime moderation during the summer. Winters are cold and very dry, with a January daily average temperature of , while summers are hot and humid, with a July daily average temperature of . The annual mean temperature is . With the monthly percent possible sunshine ranging from 45% in July to 65% in October, the area receives 2,588 hours of bright sunshine per year. A majority of the annual rainfall occurs in July and August alone. Administrative divisions The county administers 1 subdistrict, 11 towns and 3 townships. Subdistricts: * Chengqu Subdi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Luan River
The Luan River (, formerly known as ''Lei Shui'', or ''Ru Shui'') is a river in China. River The river flows northwards from its source in the province of Hebei into the province of Inner Mongolia, and then flows southeast back into Hebei to its mouth on the Bohai Sea. The headstream is known as Shandian River. This part of the river flows near the ancient Mongol capital city of Shangdu. Another important settlement in this section is Duolun. From here, the river's course turns to the southeast. Its length is about 600 km. One subsidiary is the Yixun He, which runs through Hebei. During its course, the Luan also passes by the Great Wall. After Chengde, the river is navigable. The largest city along the river's course is Chengde. Impact crater Geological evidence such as the presence of suevite suggests there is an impact crater An impact crater is a circular depression in the surface of a solid astronomical object formed by the hypervelocity impact of a smaller obje ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Mouth
A river mouth is where a river flows into a larger body of water, such as another river, a lake/reservoir, a bay/gulf, a sea, or an ocean. At the river mouth, sediments are often deposited due to the slowing of the current reducing the carrying capacity of the water. The water from a river can enter the receiving body in a variety of different ways. The motion of a river is influenced by the relative density of the river compared to the receiving water, the rotation of the earth, and any ambient motion in the receiving water, such as tides or seiches. If the river water has a higher density than the surface of the receiving water, the river water will plunge below the surface. The river water will then either form an underflow or an interflow within the lake. However, if the river water is lighter than the receiving water, as is typically the case when fresh river water flows into the sea, the river water will float along the surface of the receiving water as an overflow. Alon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Estuary
An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environments and are an example of an ecotone. Estuaries are subject both to marine influences such as tides, waves, and the influx of saline water, and to fluvial influences such as flows of freshwater and sediment. The mixing of seawater and freshwater provides high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world. Most existing estuaries formed during the Holocene epoch with the flooding of river-eroded or glacially scoured valleys when the sea level began to rise about 10,000–12,000 years ago. Estuaries are typically classified according to their geomorphological features or to water-circulation patterns. They can have many different names, such as bays, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lüshunkou District
Lüshunkou District (also Lyushunkou District; ) is a district of Dalian, Liaoning province, China. Also formerly called Lüshun City () or literally Lüshun Port (), it was formerly known as both Port Arthur (russian: Порт-Артур, translit=Port-Artur) and Ryojun ( ja, 旅順). The district's area is and its permanent population is 324,773. Lüshunkou is located at the extreme southern tip of the Liaodong Peninsula. It has an excellent natural harbor, the possession and control of which became a '' casus belli'' of the Russo-Japanese War (1904–05). Japanese and then Russian administration was established in 1895 and continued until 1905 when control was ceded to Japan. During that period, it was world-famous and was more significant than the other port on the peninsula, Dalian proper. Toponym In English-language diplomatic, news, and historical writings, it was known as Port Arthur after a British Royal Navy Lieutenant named William Arthur who surveyed the harbor i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape (geography)
In geography, a cape is a headland or a promontory of large size extending into a body of water, usually the sea.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, p. 80. . A cape usually represents a marked change in trend of the Coast, coastline, often making them important landmarks in sea navigation. This also makes them prone to natural forms of erosion, mainly tidal actions, which results in them having a relatively short geological lifespan. Capes can be formed by glaciers, volcanoes, and changes in sea level. Erosion plays a large role in each of these methods of formation. List of some well-known capes Gallery File:Cape Cornwall.jpg, Cape Cornwall, England File:Nasa photo cape fear.jpg, Satellite image of Cape Fear, North Carolina File:Cape McLear, Malawi (2499273862).jpg, Cape MacLear, Malawi File:Cape horn.png, Map depicting Cape Horn at the southernmost portion of South America File:Spain.Santander.Cabo.Mayor.jpeg, Photograph o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
