Where is Linzhou in ancient times now?

Linzhou in ancient times is now Linzhou City, Henan Province.

Linzhou in ancient times is located in the northwest of Henan Province, China, which is today's Linzhou City. Linzhou City, a county-level city under the jurisdiction of Henan Province, is hosted by Anyang City, located in the northwest of Henan Province, at the eastern foot of Taihang Mountain, at the junction of Shanxi, Hebei and Henan provinces, and adjacent to Anyang County, Hebi City and Qixian County in the east; South is connected with huixian city and Weihui City; West of Taihang Mountain Range, bordering Huguan County and Pingshun County of Shanxi Province; North and Shexian County, Hebei Province across the Zhanghe River. The total administrative area is 246 square kilometers. By 222, the total population of Linzhou is 1.16 million.

Linzhou has a long history in the history of China and was once one of the famous ancient cultural cities. It is famous for Meng Changjun, a famous politician and cultural celebrity in China during the Warring States Period. Linzhou is also rich in historical sites, such as ancient temples, city walls and cultural relics, which attract history lovers and tourists to visit.

the topography of Linzhou city:

Linzhou city is mountainous, with mountains and hills accounting for 86%. The terrain is high in the northwest and low in the southeast. The highest elevation in the territory is Sifangnao (1632 meters above sea level), the lowest elevation is located in the northeast of Wulong Town (about 2 meters above sea level), and the urban area is 36.8 meters above sea level. Linzhou is located at the eastern foot of Taihang Mountain and belongs to the North China seismic belt. There are many faults in Linzhou, most of which belong to normal faults. The largest fault is located in the west of Linzhou basin and extends to the north, with a length of 35 kilometers. The fault plane tends to the east, with an inclination of 5-8 degrees and a vertical fault distance of 1 meters.

in addition, there are 4 large faults and many small faults. Limestone, many cracks and caves are widely distributed in most parts of Linzhou, which makes surface water easily lost. Where there is a water-resisting layer, the groundwater is buried deeply, so it is quite difficult to mine. At the eastern foot of Taihang Mountain, the surface is strongly eroded, with many steep cliffs and canyons, resulting in a huge height difference between Taihang Mountain and Linzhou.