Traditional Culture Encyclopedia - Tourist attractions - Where is the most fun place in Shaanxi?

Where is the most fun place in Shaanxi?

There are too many, it depends on where in Shaanxi you want to go. There is something fun to do everywhere. You'd better go to Love Freedom and have a look. There is a lot of information on the travel website.

/portal/index/index.html

/view/6510.htm#8

Special products

Terracotta warriors and horses, Tang Sancai, Blue and white porcelain, paper-cuts, bronzes, stone carvings

Local flavor

Xifeng wine, osmanthus thick wine, Dukang wine, meat buns, glutinous rice noodles, crystal cakes, fire crystal persimmons, Lintong pomegranates , mutton steamed buns, Pucheng steamed buns, Qishan saozi noodles, five-spice donkey meat, polygonum flower sugar, millet, northern Shaanxi red dates, fried oil cake, Hanzhong rice skin, jelly, black rice, kiwi fruit, Fuji apple

< p>Scenic spots

Xi'an (known as Chang'an in ancient times) is located on the south bank of the Weihe River. In the past, many emperors used the Wei River Basin as their base. Qin Shihuang unified the Central Plains and relied on this land to supply grain, grass and horses. Therefore, this land was known as the "Eight Hundred Miles of Qinchuan". It also had Tongguan in the east, Wuguan in the south, Dashan Pass in the west, and Jincheng Pass in the north. It is called Guanzhong Plain. The passes on all sides, coupled with the two natural barriers of the Northern Shaanxi Plateau and the Qinling Mountains, make the Guanzhong Plain a "country of four fortresses", an important military base that can be attacked when advancing and defended when retreating. Since the Western Zhou Dynasty, 12 dynasties have established their capitals here, which lasted for more than 1,100 years.

Qinchuan is uniquely endowed with 800 miles of land. It is irrigated by the Wei River and has hot winds retained by the Qinling Mountains. Therefore, it has abundant heat and green land. Local people like to sing: "Pancakes are used as pot lids" and "Good girls don't marry outsiders". They say that because of the good rice and wheat, their daughters don't want to leave their hometown.

Guanzhong Basin

The Guanzhong Basin relies on the Qinling Mountains in the south and the "Beishan" in the north. It is between the Northern Shaanxi Plateau and the Qinling Mountains. Starting from Baoji Gorge in the west and ending at Tongguan Port in the east, it is about 360 kilometers long from east to west, narrow in the west and wide in the east. The total area is 39064.5 square kilometers. The Guanzhong Basin is formed by alluvial rivers and loess accumulation. It has flat terrain, fertile soil, abundant water resources, and good mechanical farming and irrigation conditions. It is the area with the best natural conditions in Shaanxi and is known as the "Eight Hundred Miles of Qinchuan". The basic landform types are river terraces and loess plateaus. The Wei River crosses the basin and flows into the Yellow River. The river channel is low and flat, with an altitude of 326 to 600 meters. From the Weihe River channel to the south and north, the terrain increases in an asymmetrical step-like manner, transitioning from first- and second-level river alluvial terraces to first- and second-level loess plateaus 200 to 500 meters higher than the Weihe River. The terraces are distributed continuously on the north bank, while on the south bank they are incomplete. Each major tributary of the Wei River also has corresponding multi-level terraces. The broad terrace plain is the most fertile area in Guanzhong. Between the secondary terraces on the north bank of the Weihe River and the northern Shaanxi Plateau, there is the Weibei loess plateau extending from east to west. The plateau is vast and generally has an altitude of 460 to 800 meters. It is the main grain-producing area in Guanzhong. The loess plateau on the south side of the Weihe River is intermittently distributed, about 250 to 400 meters higher than the Weihe River. It is in the shape of a staircase or an inclined shield, gently sloping from the northern foot of the Qinling Mountains to the Weihe River Plain, such as the Wuzhangyuan of Qishan Mountain and the Shenhe Shenhe south of Xi'an. Yuan, Shaolingyuan, Bailuyuan, Yangguoyuan in Weinan, Gaoyuanyuan in Huaxian, Mengyuan in Huayin, etc. have now developed into comprehensive agricultural zones dominated by forests and gardens.

Northern Shaanxi Mountains

Including Yulin City and Yan'an City, they are both in the north of Shaanxi, so they are called Northern Shaanxi.

Northern Shaanxi is the holy land of revolution in China. The Party Central Committee and Chairman Mao and other older generation proletarian revolutionaries lived and fought here for 13 years, leaving behind a large number of precious revolutionary cultural relics, revolutionary memorial sites and rich spiritual wealth - the revolutionary spirit of northern Shaanxi. There are more than 140 revolutionary cultural relics in the city, the most important of which are the former site of Fenghuang Mountain, the former site of Yangjialing, the former site of Zaoyuan, the former site of Wangjiaping, and Wayaobao in Zichang County (formerly the Political Bureau of the Central Committee of the Communist Party of China). The former site of the conference) and other national-level protected cultural relics. Provincial revolutionary cultural relics include: the former site of the Shaanxi-Gansu-Ningxia Border Region Government, the former site of Nanniwan in Yan'an City, the former revolutionary sites and former residences of Wuqi County, Zhidan County, Zichang County, Ansai County, Liu Zhidan Cemetery, Xie Zichang Cemetery, Luo "Old Luochuan Politburo Meeting Site" in Fengjia Village, Sichuan County, etc.

Shaannan Mountain

Including Hanzhong City, Ankang City and Shangluo City.

In the Qinba Mountains south of Guanzhong, the terrain structure of two mountains sandwiched by a river is very prominent. There is the Hanzhong Basin in the west of Qinling Mountains and Bashan, and the Ankang Basin in the east. Mainly composed of Paleozoic metamorphic complex, it is a rich area of ??agricultural and forestry specialties and non-ferrous metal resources in Shaanxi. The total area is 74,017 square kilometers.

The Qinling Mountains in Shaanxi Province are the backbone of the Qinling Mountains. The slopes are steep in the north and gentle in the south, and the mountains are majestic and majestic. The general altitude is 1,500 to 3,000 meters, which is 1,000 to 3,000 meters higher than the Guanzhong Basin and Hanzhong Basin. The main vein is distributed in the northern part of the mountainous area, with many peaks above 3,000 meters above sea level, forming the high and mid-mountain terrain of the Qinling Mountains. The glacial moraine terrain left by ancient glaciation in Taibai Mountain is well preserved. The Qinling Mountains, with Taibai Mountain as its main peak, is divided into three branches from the west. The mountains gradually become lower from the north to the south, and they have become low mountains and hills at the edge of the Hanzhong Basin. To the east of Taibai Mountain, the mountainous terrain gradually decreases. In the Shangluo area, the mountainous terrain structure separates to the east like a palm, with red fault basins and valley flats in between. There are two to three levels of terraces preserved in the basin and valley flats. The mountainous terrain is steep in the north and gentle in the south, resulting in short and sharp creeks and valleys on the north slope, and long water sources on the south slope, cutting off the east-west ridges and forming many canyons. The water resources are abundant, which provides conditions for the construction of small and medium-sized water conservancy and electric power projects.

Daba Mountain between Sichuan and Shaanxi runs northwest to southeast. It is generally 1,500 to 2,000 meters above sea level. It is more than 1,000 to 1,500 meters higher than the Han River Valley. It is about 300 kilometers long from east to west. The west of Ren River is usually called meters. Cangshan, to the east is called Dazhu Mountain. The water on the north side of Daba Mountain flows into the Han River. The upper reaches are deep canyons, and the middle and lower reaches are circuitous and open, forming many small "dams" in the mountains. There are two levels of river terraces in the Bazi, with farmland, villages and towns concentrated. Ningqiang, Nanzheng, Xixiang, Zhenba and Zhenping counties are mountainous areas composed of limestone. Karst terrains such as rock buds, karst ditches, sinkholes, caves, and underground rivers are developed. Surface water is scarce but groundwater is abundant. To the west of the Hanjiang Valley lies the low mountain and hilly area of ??the upper reaches of the Jialing River. The terrain is gentle and the valley is relatively open. It is the main water and land channel between Shaanxi and Sichuan.