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Lianjiang River Basin Overview
The upper reaches of Jixi County is the upper reaches of Lianjiang River, including middle mountains, low mountains and hilly areas. The main ridge trend and basin valley extension direction are generally south-west or north-east. There are many types of geomorphological units. The river source zone is a mountainous area with the main peak above 1,000 meters above sea level, distributed in Dazhan Mountain in the east, Assembly Mountain in the west and Huishan Mountain in the middle. The valleys are deep and winding, including Renmen Canyon, Dazhan Canyon, Xiaoyao Canyon, Tongyuan Canyon, Shanyun Canyon, Huangbaao Canyon and Huixi Canyon. Downstream, there are low mountainous areas first, with the main peak above 500 meters above sea level and the lowest altitude 400 meters above sea level. Distributed in the extended area of ??Zhongshan. The depth of the valley is generally 200 to 400 meters, including Dayuan Canyon, Wangjiayuan Canyon, Yangxiyuan Canyon, Longcongyuan Canyon, Bingkengyuan Canyon, Gexiyuan Canyon, etc. Hills, with an altitude below 500 meters, most of which are around 300 meters above sea level. It is composed of sandstone, shale and medium-coarse-grained granite. It is mainly red soil, mostly agricultural vegetation, and dry gardens are scattered throughout. Some of the hill tops are turtle-backed or round-shaped, with small slopes and surface weathered crusts can be seen in many places. In the higher areas, gullies are developed, water erosion is significant, and a small amount of alluvial and flood sediments accumulate on both sides of the stream. Basin valleys are mainly distributed along rivers. Areas that have been faulted or descended due to crustal movement have become places where water gathers and flows through. Long-term scouring and erosion by running water lowers and widens the terrain, entraining a large amount of sediment to form a floodplain, which gradually evolves into terraces or alluvial fans, which continue to expand and connect with each other, and finally form intermountain basins and valleys. The outer edges of basin valleys are mostly connected with low mountains or middle mountains. The larger basins include Huayang Basin, Lukunchang Basin, Jingzhou Basin, Fuling Basin, Hujia Basin, Banqiao Basin, Fengtou Alluvial Fan, and Huixi Alluvial Fan. Fan, Pingyin alluvial fan, etc.; the larger valleys include Dengyuan Valley, Jinsha Valley, Kongling Valley, Longxi Valley, etc.
Downstream She County is located in the mountainous area of ??southern Anhui. It has tall and straight peaks, winding mountains, undulating hills, crisscrossing valleys, and diverse landforms. The Huangshan Mountains tower in the northwest, and the Tianmu-Baiji Mountains form a barrier. In the southeast, Jianjiang, Xin'anjiang Valley and Lianjiang Valley are the junction of two major mountain systems. The main landform types are: Zhongshan. There are three mid-mountain terrain areas: Huangshan Mountain, Tianmu Mountain and Baiji Mountain, which are respectively distributed in the northwest, northeast, southeast and the border areas with neighboring counties. The surface of the area is strongly cut, with steep slopes, staggered rocks, crisscross ravines, high mountains and deep valleys, and mostly mountain tops. Pointed shape, the bottom of the valley is mostly V-shaped. The mountain is composed of granite, rhyolite, andesite, sandstone, phyllite and other rocks. Low mountains, with an altitude of 635-1000 meters, and a relatively high altitude of more than 300 meters. Low mountains with greater undulations are mainly distributed in the peripheral areas of Zhongshan. The mountains are steep and have the same rock composition as Zhongshan. Low mountains with smaller undulations are mainly distributed in the transition zone from mountains to hills or basins. The mountains are smaller and the slopes are gentler. , the rock composition includes granite, epimetamorphic rock, sandstone, and limestone, with a total area of ??166.56 square kilometers. High hills, with an altitude of less than 635 meters and a relatively high altitude of 200-300 meters. Mainly distributed in the outer edges of low mountains and the inner sides of basins and valleys. It is composed of sandy phyllite, phyllite sandstone, and clastic rock. The top of the hill is blunt and pointed, maintaining a certain direction of the hill ridge, and the general slope is about 30 degrees. Low hills, with an altitude of less than 550 meters and a relative height of less than 200 meters, are mainly distributed in mountain basins, inside and at the bottom of valleys. The rock composition is mainly light metamorphic rock, limestone, and red sandy conglomerate, spreading in an east-west direction, with gentle hill tops. , strongly denuded, mostly round, partially exposed, with a slope less than 20 degrees. In valleys, the altitude is generally less than 200 meters. Most of them are distributed in strips. The Lianjiang Valley covers an area of ??112.50 square kilometers. It is located in a sag basin in the ancient Jiangnan continent. The Jurassic and Cretaceous strata form the base of the accumulation. The valley is deeply cut, and bedrock is often exposed at the bottom. On both sides of the river It is a multi-level terrace composed of alluvial gravel and multi-stage accumulations. Upstream Jixi County is located near 30° north latitude, more than 160 kilometers away from the East China Sea to the east, and has a north subtropical monsoon climate. The territory is mountainous and the terrain is relatively high. Affected by the terrain, compared with plain areas at the same latitude, the temperature is lower, the precipitation is more, the sunshine is less, the wind is weaker, and it shows vertical differentiation. In spring, the temperature rises quickly and there are many rainy days; in autumn, the temperature drops quickly and there are few rainy days. Spring and autumn are short seasons, which are actually the transitional seasons between winter and summer.
The lower reaches mainly have a humid monsoon climate on the northern edge of the subtropical zone. Spring, from March 16 to May 20, lasts for 66 days. During the season, the wind direction and temperature change frequently, from warm to cold, from cloudy to sunny, which is the season with the most changes in weather. This is the result of the intense struggle between the warm and cold air currents from the north and the south, advancing and retreating, creating a see-saw situation.
According to analysis of meteorological data for many years, in early spring, warm and humid air from the Pacific Ocean begins to advance from south to north, forming a season of spring warmth and flower blooming. However, cold air from the north is still moving south frequently, often expelling warm air around the Spring Equinox and Qingming Festival, forming the "Qingming Festival" A low-temperature, rainy climate with heavy rains. Summer lasts from May 21st to September 25th, lasting 128 days. During the season, the temperature gradually rises, the warm and humid air flow is controlled, and the plum rain is significant; after entering midsummer, the weather is hot, large-scale rainfall is rare, southerly winds and local thundershowers are common, and the temperature and humidity are high and humid. This is the season when plants and crops grow most vigorously. . In some years, heavy rains are concentrated, resulting in floods, or persistent drought and high temperatures result in droughts. Autumn lasts from September 26 to November 20, lasting 56 days. During the season, although the temperature shows a downward trend, it is still 1-2°C higher than the spring temperature. Most of the autumn weather is crisp, sunny and less rainy, and the temperature is relatively stable. The average rainfall only accounts for 14% of the annual rainfall, and the rainy days only account for 20% of the annual rainy days, which is conducive to the flowering and harvesting of crops. After the cool days of autumn, due to the influence of the return of the sun, there are often "September Double Ninth Festival" and "October Xiaoyangchun" warm weather; and because the cold air begins to move southward, there are also autumnal equinox cold weather with bleak autumn wind and continuous autumn rain. Winter lasts from November 21st to March 15th of the following year, which lasts for 115 days. During the season, the cold air from the north moves southward, causing the temperature to drop sharply. The temperature drop in December has been 5.9℃. The seasonal average temperature over the years is 5.6°C, and the number of days below freezing is 12. The general trend is that cold air takes the lead, and the climate is less rainy and cold, with more northwesterly winds. Heavy snow, extremely cold weather, and dry wind freezing mostly occur in the cold weather of March and September. Jixi County is located in Huayang Town. According to Jixi County Chronicles written by Emperor Qianlong of the Qing Dynasty, Huayang Town was "established by the Han Dynasty, and today's towns are all the same." It has been the seat of the county since it was established. It is located in the south-central part of the county. The Yangzhi River flows through the entire territory from northeast to southwest; it covers an area of ??33 square kilometers. There are low mountains in the north and east, hills in the west and south, and a basin in the middle. The territory is the main industrial belt of Jixi, with 774 county and town enterprises in machinery, chain, cement, fertilizer, silk reeling, silk weaving, building materials, clothing, furniture, printing, Huizhou ink, etc. The Anhui-Jiangxi Railway and Wutun Highway run parallel to each other, and county and township highways radiate in all directions, making the transportation convenient. It is the political, economic, cultural and educational center of the county. The county seat is located at the intersection of Huixi River and Ruxi River flowing into Yangzhi River. In the fifth year of Qianlong's reign in the Song Dynasty, which was the sixth year of Li Yu's reign in the Southern Tang Dynasty (967), the city wall was built. The city is oval in shape, pillowed on Wulong Ridge in the north, facing Long () Field in the south, spanning Guanshan and Mashan in the west, and facing Yangzhi River in the east. The Jixi County Committee of the Communist Party of China, the County People's Government, the County People's Congress, and the County CPPCC are located in North Street. The town people's government is located on Huancheng East Road.
The county seat of Shexian County is located in the town of Huizhou. It is located in the middle of the county, where mountains and rivers gather. It leans on mountains to the east and faces water on three sides to the north and southwest. The east is the ancient county town, which is a small basin in the mountains; the west is the ancient Fucheng, separated from the ancient county town by Doushan and Changqing Mountains (i.e. Wuliao Mountain). The four rivers Fengle, Fuzi, Bushe and Yang merge here to form the Lianjiang River, which then flows eastward and flows into the Xin'an River. The Wenzheng Mountain Range meanders eastward from then on, connecting with the Tianmu Mountain Range. The city site is "dangerous in mountains and rivers, and it was created by nature." Huicheng has a long history. According to the Tang Dynasty's "Yuanhe Prefecture and County Chronicles", at the end of the Eastern Han Dynasty, there was the ancient city of Mao Gan in Wuliao Mountain. From the late Han Dynasty to the Sui Dynasty, there is no record of changing the county seat. At the end of the Sui Dynasty, Wang Hua of Yining Zhong raised troops to protect the territory, moved the county government from Wansui Mountain in Xiuning County, and built the county city at the former site of Maogan City.
After that, in the nearly 1,300 years to the end of the Qing Dynasty, it has been a county, a state, a road, and a city. The county government was attached to Guo Wucheng for nearly 1,000 years, until the county magistrate Shi Guifang initiated the construction of it in the 34th year of Jiajing in the Ming Dynasty (1555). The county seat was built in 1939. The county government was no longer attached to Guo. After the founding of the People's Republic of China, in order to facilitate transportation, the large and small north gates and Desheng Gate in the Fucheng, and the Ziyang Gate and Yuping Gate in the county were successively demolished. Only the Chaoshui West Gate and Yuecheng Gate in the Fucheng, and the Xin'an and Wenzheng gates in the county were left. It still exists, and some of the prefecture and county walls are still preserved. After 1979, in order to protect the ancient city, a new area was built in the west of the city. The town was established in the 21st year of the Republic of China (1932), and Baojia was established under the town. In 1932, there were 7 security guards in Fucheng, including Yanghe, Zhongcheng, Huangshan, Beijie, Dooshan, South Street and West Street, 2 security guards in Shanglu and Xinmin in the county, and 3 security guards in Xiguan, Beiguan and Guguan outside the city. After the founding of the People's Republic of China, the Baojia system was abolished and streets were established under the town. In 1950, 4 streets were established in the prefecture: Southwest, Zhonghe, Xinbei, and Doosan. The county seat was established in 1 Xinlu Street. Outside the city, there were 5 Xiguan, Beiguan, Zhongjie, Nangong, and Xin'an Streets. sub-districts, and an administrative village in Wenzheng; in 1958, the town was converted into a commune; in 1965, the town organizational system was restored. The Longchuan Hu Ancestral Hall is located in the south of Dakengkou Village, Yingzhou Township, Jixi County. Dakengkou was called Longchuan in ancient times.
The ancestral hall was first built in the Song Dynasty, rebuilt during the Jiajing period of the Ming Dynasty, and rebuilt in the 24th year of the reign of Emperor Guangxu of the Qing Dynasty (1898). The ancestral hall covers an area of ??1,564 square meters, with a length-to-width ratio of 2:1. The square, pillars, railings, flag foundation stones and terraces in front of the temple are all made of granite. To the south, Zhaobi is across the Longchuan River, with bluestone bridges on the left and right. Three entrances and seven bays. The forward gate tower has a double-eaves and mountain-like structure, 8 corners, 5 steps, and a width of 22 meters. The instrument gate is 2.3 meters high and 3.4 meters wide. Stone drums and stone lions confront each other in front of the door. There are 10 square stone pillars, 5 moon beams and 4 forehead beams in the front and rear directions of the gatehouse. The patio behind the gatehouse is 13.77 meters deep and 13.10 meters wide. There are 12 square stone pillars and 24 moon beams in the east and west corridors. Climb the 4 steps beyond the patio to enter the main ceremony hall, which is 17.47 meters deep, 22.16 meters wide, and 9.3 meters high at the top. 14 ginkgo columns with a circumference of 1.66 meters and 12 winter melon beams of different sizes form the roof truss. The column is supported by lotus-shaped jujube wood pillars and octagonal stone slabs. There are 12 floor-to-ceiling partition doors with a height of 3.68 meters in the east and west sequence. There were originally 24 fans in the upper part, half of which remain today. There are two floors of the Xiangtang at the back, with a long and narrow patio in front. There are 24 floor-to-ceiling partition doors in the east and west corridors with a height of 2.65 meters. A plaque with the words "Ancestral Hall of the Hu Family in Longchuan" written by Wen Zhengming of the Ming Dynasty originally hung on the gatehouse; a plaque with the word "Ancestral Hall" originally hung in front of the main hall was inscribed with "King Guangzhuang in the last years of Jiajing Ding" (uncle of Emperor Jiajing). Two wooden couplets originally hung in front of the main hall. The plaques and couplets were removed during the Cultural Revolution. The overall building integrates bricks, wood and stone carvings, and is especially famous for its wood carvings that are "plentiful, refined and beautiful". There are shallow floating, deep floating, hollow, matching floating and hollow, and both line and floating. The content is a collection of auspicious birds and animals, flowers, plants, bamboos, mountains, rivers and clouds, celestial bodies and aquariums, pavilions, dramas and stories, ancient characters, customs and customs. Experts call it the "Wood Carving Art Hall". In October 1982, it was announced as a county-level key cultural relics protection unit. In July 1986, it was upgraded to a provincial key cultural relics protection unit. The State Administration of Cultural Heritage allocated 95,000 yuan for renovation and advancement from November 1987 to September 12 of the following year. It was later upgraded to a national key cultural relics protection unit.
Hu Shi’s former residence is in Shangzhuang Village, Jixi County. It was built in the 23rd year of Guangxu reign of Qing Dynasty (187 AD). The main house faces south, with brick and wood structure, two entrances and three hatchbacks, and a "back"-shaped building. It covers an area of ??208 square meters and has a construction area of ??350 square meters. The facade has two pillars and a single door on the first floor, with brick carvings and owl kisses on it. In front of the door, there is a wooden sign with gold characters on a black background "Hu Shi's Former Residence", inscribed by contemporary calligrapher Sha Menghai. The furnishings in front of the entrance hall are as before, including a table, an Eight Immortals table, and a Taishi chair. A banner reading "Hu Shi's Former Residence" hangs above, and a middle-aged portrait of Hu Shi hangs below. On both sides there are couplets: "Walking thousands of miles and half of the world, with eyes so high that there is no one in the world." Qian Juntao wrote. Coffee tables and armchairs are arranged in the east and west, and a chart of Hu Shi's immediate family is hung on the wall. In the west is the wedding room of Hu Shi and Jiang Dongxiu. There are wooden beds, tables, chairs, cupboards, stools, etc. in the room. The front room was Hu Shi's childhood reading room. The eastern room and the wing room were used by Hu Jue (the second brother of Hu Shi). The two rooms in the main hall display the manuscripts of Hu Shi's family letters and some of his works, Hu's genealogy, calligraphy and paintings, poems donated by celebrities at home and abroad, and Hu Shi's "family portrait" photos. The back hall is shallow in depth. There is an iron flower portrait of Hu Shi's father hanging in front of the hall, and a photo of Hu Shi's biological mother Feng Shundi on the east side. There is a huge plaque with gold characters on the red background hanging on it. The four characters "Zhijie Xuanwei" are written by Cheng Dongping, a native of Yi, and the inscription is "Given by Zhu Yayun, Magistrate of Jixi County, in the 31st year of the Republic of China." In the former residence, 12 floor-to-ceiling partition doors are inscribed with orchids, and 4 window lattice panels are engraved with flowers and inscriptions. They were made by Hu Guobin, a master of ink modeling. The former residence also displays photos of Hu Shi in various periods. Hu Shi's handwritten scroll "On the Destruction of Gods" written by Fan Zhen. Zhang Zhidong presented Hu Tiehua hat tube, Hu Tiehua seven-star sword, imperial edict box and conches brought back from Taiwan. The back hall is connected to the kitchen in the east. In September 1986, it was listed as a key cultural relic protection unit at the county level. In November of the following year, the county people's government allocated funds for repairs, and it was opened to the domestic market in December.
Xiao Jiuhua is located in the northeast of Jingzhou Township, Jixi County. The mountains and rivers are secluded, and it is said that "Jiuhua Mountain Ksitigarbha once practiced hard here, hence its name" ("Chinese Famous Places Dictionary Anhui Volume"). Xiaojiuhua Mountain is abrupt and has deep ravines, like several dragons meandering together. There is a hill in the middle, where the river twists and turns, shaped like a peninsula, with the Ksitigarbha Hall on it. The mountains on the other side are lined like a screen, and in front is the Yinping Temple. There are two strange peaks nearby: one is in the northeast of the Qiu, with dangerous rocks tilted in three stacks, like multiple towers and pavilions, with waterfalls flowing up and people walking down; the other is in the northwest of the Qiu, with stone peaks protruding from the river bend, with sharp tops and sides, and a curved middle. , round and long at the bottom, with grass growing around the waist like a hanging tassel. The curved ring resembles a knife, commonly known as "Guan Wang Dao". The blade is 39 meters high. The four characters in the ancient book on the front "will never be worn out" have been lost for a long time. In the leap seventh month of the lunar calendar in the 27th year of the Republic of China (1938), Hu Zhongwu, a local, contributed money and wrote "Juqi Commemoration" on it.
In October 1965, three people including Zhuangzi villager Zhang Bijin wrote a huge slogan "Long Live the Communist Party of China" on the peak. The rocks along the river are intertwined and cross-sectioned like dams. There are many natural caves and deep pools, commonly known as "Nine Wells and Eighteen Dams", including several iron cauldron pools. There are ten sceneries in Xiaojiuhua: the deep iron cauldron, the green screen dripping green, the blade of a knife sticking into the clouds, the Hengyan Waterfall, the lion's mouth roaring to the sky, the misty rain in Shuangxi, the five dragons grabbing the pearl, the twilight mist on the peak, the sweet spring in Jiujing, and the early snow in Meigan. There are many inscriptions and chants in the past dynasties. During the "Cultural Revolution", all palaces, temples and Buddhist statues were destroyed. Today, the beautiful mountains and rivers remain the same, and it is still a good place for tourism and summer vacation.
The first pass in the south of the Yangtze River, also known as Yaoyao Rock. In the east of Fuling Township, Jixi County, it has an altitude of 424 meters. It is an important pass on the Huihang Ancient Road and the main passage of Qingliang Peak. Guanjiao Yankou Pavilion has the inscription "A Path Leads to Jiangsu and Zhejiang" in Wei style. Crossing the first bridge in the south of the Yangtze River, climbing up the pass from the west, you will see steep mountains and craggy rocks, among which the Mopan Stone, Tianguan Stone, Jiangjun Stone and Rice Rice Husk are the most amazing. There are giant peaks of rock standing between the north and the south, with a ravine in the middle and a free river meandering between them. About 2 meters long granite slabs are embedded in the northern rock wall to build a plank road, with some stone strips half suspended in the air. There is a hole in the sky at the top, which is the pass. From the foot of the rock to this point, there are more than 1,400 levels. First time climbers feel palpitated and dizzy, walking slowly against the wall and not daring to look down. There are rocks in the stream, stacked heavily like animals and melons. The water in the stream is ups and downs, singing softly and roaring, sometimes trickling elegantly, sometimes rushing into a pool. The gate is composed of four large stone bars horizontally framed by natural rocks. The lintel is engraved with "The First Pass in the South of the Yangtze River" in the west, and "Shao Daotang Title was built by people in the second year of Tongzhi in Huihang Suoyue" in regular characters in the east. The door is closed, and the mountain wind is hunting, as if flying in the sky. After entering the pass, the stone path is slightly flat, but still spirals between the steep walls. On the rock wall next to the Shicha Pavilion in Guandong, there is a brief history of the ancient road engraved: During the Baoyou period of Song Dynasty (1253-1257), Hu Dan carved the big stone gate into stone blocks according to the mountain terrain, which were more than five miles away to facilitate travel. During the Dade period of the Yuan Dynasty (1297-1307), the Cheng family of Beixiang (today's Beicun) regarded the terrain as dangerous, so they cut down stones again to form barriers to block the side, making travel safer. During the Chenghuajian period of the Ming Dynasty (1465-1487), Wang Yimao and others rebuilt it. It has been repaired in subsequent dynasties. After the founding of the People's Republic of China, nearby villagers made an agreement to organize maintenance to this day. There is the "Er Cheng" temple in the pass, built by Hu Guisen of Hujia Village. It is said that in the spring of the 21st year of the Republic of China (1932), Cheng Zaoqi and Cheng Ruihu of Beicun went to Zhejiang to do business. They took shelter from the rain and hung under a rock. They all died when the rock collapsed, so they built a temple to express their condolences. Later, Shao Zaibing funded the construction of a stone pavilion next to it. The origin of the name of the first pass in the south of the Yangtze River: According to legend, Li Shixian, the servant king of the Taiping Heavenly Kingdom, led his troops to pass here in 1861 and praised the natural danger and named it; one theory is that it was named by Hu Zongxian in the Ming Dynasty.
Dazhang Mountain (Dazhang Mountain) belongs to the Tianmu Mountains and stretches between Dazhang and Xiaoyao Township in Jixi County today. There are more than 50 peaks above 1,000 meters above sea level. They are collectively called Dazhang Mountain and cover an area of ??nearly 80 square kilometers. Both "Shan Hai Jing" and "Xiang Fu Jing" say: Santianzi Zhangshan is also known as Santianzidu, Sanwang Mountain and Yushan. The mountains and rivers of Dazhang "divide into three branches under the daytime pool, connecting the three cities of Jinling, Gusu and Lin'an, and ending at the sea. That's why Zhangshan is called the capital of the three emperors." (Qing Dynasty, "Liu Sheng Tang Ji" written by Zhou Zan, Huizhou's edict). Legend has it that in ancient times, the Yellow Emperor, Rong Chengzi and Fuqiu Gong came to the mountains to collect medicine and make elixirs. In the Spring and Autumn Period, Wu and Yue were separated here, and Zhang County in Qin Dynasty was named after the mountain. "Zhangshan Mountain is covered with greenery" is a scene in ancient Huayang. There are monuments such as the Tomb of the Emperor and the Tomb of the Prime Minister in the mountain. The main peak, Qingliang Peak (known as Zhangfeng in ancient times), is located in the southeast corner of Xiaoyao Township, with an altitude of 1,787.4 meters. It is the highest peak in the Tianmu Mountains and the highest point in the county. It is majestic and has deep ravines. The terrain entering the mountain from the first pass in Jiangnan is relatively gentle. The natural ecology is complete, with more than 1,000 species of seed plants in 120 families, 31 species of which are nationally protected plants; and rich in animals, 13 species including black muntjac, sika deer, leopard, clouded leopard and white-necked pheasant are nationally protected animals. It is known as the "Grand View Garden" of another creature in East China. Strange pines, strange rocks, sea of ??clouds and Tianchi are the four wonders of Qingliang Peak. There are Liming Point, Shemu Empress Point, Stage Top, Baili Rock, Baizhang Rock, Crucian Ridge, Kitchen Knife Back, Topknot Stone, Gassho Stone, Camel Stone, Lion Stone, Guanyin Stone, Immortal Boating, Golden Turtle Watching Heaven Gate, Monk Scenic spots such as the Nun on the Back, the Eighteen Dragon Pond, the Welcome Pine, and the Qilong Pine. There are many "small plains" on the top of the peak, ranging from five to six acres in size to more than an acre in size, with thickets of arrow bamboos, flowing springs and waterfalls, and endless pools, including giant salamander and willow leaf fish. On a clear day, you can see thousands of peaks competing in the distance. When it clears up after the rain, the "Buddha's light" often appears. The origin of the mountain’s name: In the summer of 1953, Soviet experts from the Huizhou garrison climbed to the main peak to survey and named it after the climate characteristics. Later, relevant county departments organized multiple inspections. In 1985, more than 20 scientific and technological personnel from the province, prefecture and county jointly formed the "Jixi County Qingliangfeng Natural Resources Comprehensive Scientific Expedition Team". From May 17 to June 7, they conducted an inspection of the 45,000-acre mountain field on the north slope and summit of Qingliangfeng. Comprehensive inspection. In February 1986, the Anhui Provincial Government approved it as a nature reserve.
Xiqian, the Yangzhi, Bushe, Fuzi, and Fengle rivers converge in the west of Shexian County, flowing straight like Lian. When they reach the south of the city, they spread out and accumulate, and Jingchuan is green. It is called Xixi. Dry. Qian, the bank, Xigan, the bank west of the river. Piyun Peak, Chengyang Mountain, Ziyang Mountain and Longjing Mountain are surrounded by hills and green trees. Taiping and Ziyang Bridges are reflected on the left and right, and the long embankment with weeping willows surrounds the city. Chengyang Mountain was the place where Xu Xuanping lived in seclusion during the Tang Dynasty. Ziyang Mountain was the place where Zhu Xi and his son studied and lectured in the Song Dynasty. Piyun Peak is famous for Xin'an Ancient Temple. In the second year of Zhide (757) of the Tang Dynasty, 24 monasteries were built. At the end of Zhenyuan, Piyun Pavilion was built. Later, pagodas were built, temples were built, pavilions were built, and roads were paved. It was a tourist attraction in ancient She. After the Song and Yuan Dynasties, tours and poetry gatherings were particularly popular, and there were many poems and poems. Xu Chengyao compiled seven volumes of "Xi Gan Zhi". The existing tomb of Wang Caibai was built in the Republic of China, the Ancient Piyun Road and Piyun Pavilion were built in the Republic of China, the Changqing Temple Pagoda was built in the Song Dynasty, and the Tomb of Jianjiang was built in the Qing Dynasty. The two-story Piyun Pavilion is also known as the Lookout Pavilion. When you look down from the pavilion, you can see green mountains, water like a ribbon, and bridges like a rainbow. You can have a panoramic view of the ancient city. Looking far into the distance, the towering peaks of Huangshan Mountain, a hundred miles away, are faintly visible. Leaning on the railing and nostalgic for the past, my thoughts are leisurely.
Yuliang Ancient Street is close to mountains and rivers. The Xin'an Ancient Road, which is similar to the architectural style of the ancient Great Wall, connects the ancient city and Yuliang together. The Xin'an Ancient Road was the only way for Huizhou merchants in the Ming and Qing Dynasties to travel to and from Huizhou. Yuliang was one of the important waterway docks in ancient Huizhou, and Yuliang Commercial Street was formed as a result. Yuliang Street winds for one kilometer, with cobblestones of the same color arranged in an orderly manner, commonly known as Fish Scale Street; wooden houses of the same color are located on both sides of the street, with heavy buildings and overhanging eaves, lined up in rows, covering more than half of the street. Standing on the street and looking up, The blue sky seems to be a line; the old-style storefronts with the same color, various shops and shops still have their ancient appearance. The Yuliang Dam in the south of the street is a major water conservancy project in Gushe and a major landscape of Yuliang. Under the dam, there are flying beads and jade, and the snow waves are rolling, which is a spectacular sight. Walk a hundred stone steps from Yuliang Dam to the shore, cross Wangxian Bridge and arrive at Xin'an Pass, the first pass in Xin'an. After leaving Xin'an Pass and crossing Ziyang Bridge, you will go to Ziyang Mountain where Zhu Songjielu, the father of Neo-Confucian master Zhu Xi, gave lectures. Ziyang Academy was built here in the Ming Dynasty.
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