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广西地处北纬20°54′(斜阳岛)至26°21′,跨北回归线,属亚热季风区。在地理上,北倚五岭山脉,西靠云贵高原,东南面向南海,呈西北高而东南低的地势。境内河道密布,主要属珠江水系,河流一般由西北或北,流向南,再转向东,汇流于梧州,流经广东省入海。根据地质地理研究,在第四纪以前,由于多次长期的海水浸入,生成广泛的石灰岩。石灰岩经地面和地下水的浸蚀,发育成典型的岩溶地貌,地面溶洞很多。大河两岸又形成许多丘陵山地和大大小小的冲积平原。近一百万年来,气候温暖,雨水充足,森林茂密,动物繁多,自然资源十分丰富,很适合于原始人类的生活。
Guangxi is located at latitude 20 ° 54 ’(Slopeang Island) to 26 ° 21’ north of Guangxi and crosses the Tropic of Cancer in the tropic monsoon region. Geographically, the north relies on the Wuling Mountains, the Yunnan-Guizhou Plateau to the west, and the southeast to the South China Sea. It is high in the northwest and low in the southeast. The territory of the river is densely covered, mainly belonging to the Pearl River system, the river generally from the northwest or north, flow to the south, then turn to the east, confluence in Wuzhou, flowing through the Guangdong Province into the sea. According to geo-geography research, a wide range of limestone was formed before the Quaternary because of many long-term seawater intrusion. Limestone erosion by the ground and groundwater, developed into a typical karst topography, many ground caves. The formation of many hilly mountains and large alluvial plains on both sides of the river. Nearly one million years, the climate is warm, abundant rainfall, dense forests, animal diversity, natural resources are very rich, very suitable for primitive human life.