Which province does Maoming City belong to?

Maoming is a city in Guangdong Province. Maoming, a prefecture-level city in Guangdong Province. It is located on the coast of the South China Sea, in the southwest of Guangdong Province, with its back to the southwest of the motherland. Maonan District, Dianbai District, Gaozhou City, Huazhou City, and Xinyi City. Topography: Maoming City is backed by mountains and faces the sea. It is high in the north and low in the south, sloping from northeast to southwest. The highest point is 1,704 meters above sea level, and the lowest point is 1.6 meters above sea level. and the three major mountain ranges of Yunkai, Goulou and Wuyun in the north and northeast. Rivers crisscross the area, forming a unique landscape of mountains, hills, terraces and plains. The mountainous area is mainly composed of Yunkai Mountain in the north, Yunshan Mountain in the northeast and Goulou Mountain in the northwest. There are 1,300 square kilometers of mountainous areas above 500 meters above sea level in the junction area between the southeast of Yixin and the northeast of Gaozhou. The main peak, Datianding, is 1,704 meters above sea level, making it the second highest peak in Guangdong Province. Quilting (the junction of Gaozhou and Xinyi) is 1,627 meters above sea level, and Efenghuang (the junction of Dianbai and Yangchun) is 1,337 meters above sea level. This mountainous area forms the northern barrier of the city, blocking the flow of cold air from the north in winter and mitigating the harm of cold currents to the headquarters. In spring and summer, the warm mass from the south rises, resulting in abundant rainfall in the mountainous areas in the southern part of our city. The mountainous area has many rivers and abundant water resources. It is a major area for forestry and hydropower development. Climate Maoming City is located south of the Tropic of Cancer and belongs to the subtropical monsoon climate zone with obvious monsoons and diverse climate types. Northerly winds prevail in winter and southeasterly winds prevail in summer. The main climate characteristics are: first, there is no severe cold in winter, no scorching heat in summer, long summer and short winter, abundant heat, abundant rainfall, and obvious dry and wet seasons; second, the terrain is high in the north and low in the south, with mountainous areas in the north, large vertical temperature differences, abundant precipitation in the mountainous areas, and micro-climate characteristics. The topography and climate are complex and diverse, and the three-dimensional climate is obvious; third, there are two rainy seasons, the first flood season from April to June, which belongs to the polar front rain belt precipitation, and the second flood season from July to September, with many typhoons and other low-latitude tropical Weather system precipitation. Fourth, climate resources are abundant and meteorological disasters are frequent and severe.