Tianshui family belongs to Tianshui City, Gansu Province, and Tianshui family refers to the aristocratic family of ancient Zhao. Tianshui Zhao is a famous Zhao family, and the dream of revitalization is another world sigh. After Qin destroyed Zhao, Zhao scattered all over the country, taking the country as his surname. Before the establishment of the Northern Song Dynasty, Zhao, who was "assisted by Xirong and lived in Tianshui", was a noble family.
The Zhao family was appointed Marquis in the Han Dynasty and was worshipped in the Tang Dynasty. It was not until Zhao seized the world and established the Song Dynasty that Zhao's aristocratic position in Tianshui was replaced by Zhao Songzong. There are national, provincial and municipal key protected cultural relics 169 in China, among which Maijishan Grottoes, a world cultural heritage, is one of the four largest grottoes in China and is known as the "Oriental Sculpture Art Exhibition Hall".
A noble family is a family with a prominent family background and has been an official for generations. A family is a big family with several generations living together. These generations of big families are all families. From Mencius Teng Wengong.
Brief Introduction of Tianshui City, Gansu Province
Tianshui City is a prefecture-level city under the jurisdiction of Gansu Province, located in the southeast of Gansu Province, which governs five counties of Qin Zhou, McKee, Wushan, Gangu, Qin 'an, Qingshui and Zhangjiachuan Hui Autonomous County and national economic and technological development zones.
Tianshui, a famous historical and cultural city in China, is characterized by numerous mountains, high terrain in the northwest and low terrain in the southeast, with an altitude of 1000-2 100 meters. The highest peak field beam, up to 3 120 meters; Niubei Village, the lowest point, is 760 meters above sea level. Tianshui landform has obvious regional differentiation. The eastern and southern parts were uplifted by the folds of ancient strata, forming mountain landforms.
Due to geological subsidence and red and loess layer deposition in the north, loess layer deposition is formed, forming loess hilly landform. Due to the fracture of the banded structural belt, the Weihe Graben was formed in a small part of central China, and the Weihe River Valley landform was formed after the separation and erosion accumulation of rivers in Quaternary.