Qinzhou is a land-sea node city of the "Belt and Road" southbound passage. Qinzhou has an excellent deep-water harbor-Qinzhou Port, which has obvious location advantages. With the construction of the new land-sea passage in the west, Qinzhou's economy has taken off to the sea, injecting more vitality and vitality into this livable coastal city. At this time, Qinzhou, with complete infrastructure and sufficient development momentum, is a good time to invest in home ownership!

Qinzhou's economic development to the sea is in full swing. The Zhongma Plaza and the International Gulf City in Qinzhou Port Area are close to the Zhongma Industrial Park, attracting high-quality ecology, multiculturalism, rich products and innovative industries as the core, forming an ASEAN international business complex, which is the most suitable choice for investment and home ownership.

Introduction of geology and geomorphology in Qinzhou;

Qinzhou city is located at the southern end of Nanhua paraplatform, with complex geological structure and well-developed strata, with the most developed Paleozoic Silurian below the exposed strata. Magmatic rocks are mainly acid intrusive rocks, mainly granite and rhyolite; Fold and fault structures are developed with obvious zonation, and there are conditions for moderate earthquakes.

Qinzhou city is slightly square in shape, mainly belonging to hilly landform type. The territory is surrounded by mountains and arches in the east, west and north, with rolling hills and complex terrain. The northwest is subordinate to the mountainous area, with 100,000 mountains as the main body. The mountains are tall and green, and the waterfalls are deep. The northern and western parts belong to the hilly areas, except for a few mountainous areas and high hills, the general elevation is about 250 meters.

In the middle part, there are low hills, platforms, basins and river valley alluvial plains, mainly low hills and river valley plains, and the land is slightly flat; The eastern part is a low hilly area; The southern part belongs to low hills, coastal hills and plains, with the largest alluvial plain in the city-Qinjiang Delta.

The terrain of the whole territory is high in the northwest and northeast, inclining from north to south, and the terrain in the south drops significantly. Qinzhou mountainous area (above 500 meters above sea level) 10.08 square kilometers, accounting for 0.22%; The middle and high hills (elevation100-500m) are 686.83 square kilometers, accounting for14.75%; The low hills (below 100 meters) are 2835.52 square kilometers, accounting for 60.89%.

Platforms and terraces are 44 1.99 square kilometers, accounting for 9.49%; Plain (0-10m) is 473.3 square kilometers, accounting for10.16%; Waters (rivers, reservoirs, etc.) 108.53 square kilometers, accounting for 2.33%; Other 100.78 km2, accounting for 2.16%.

Reference to the above content: Baidu Encyclopedia-Qinzhou City