Compulsory education in Baiyun District:
1997 10 According to the "Opinions on Consolidating and Improving the Popularization of Nine-year Compulsory Education" forwarded by the General Office of the Guangdong Provincial Government, Baiyun District has strengthened the macro guidance and supervision of primary education, and incorporated several indicators reflecting the popularization into the annual work assessment of the town by the district government.
Primary school-age children are 6 years old (1997) and 10. By 2000, the whole region was enrolled at the age of 6. In 2000, the enrollment rate of school-age children was 99.7%, and the school year consolidation rate was 95.5%. /kloc-the completion rate of primary education at the age of 0/5 is 99.63%; The abnormal dropout rate of primary school students is 0.009%, which is far lower than the provincial 1%.
High school education:
Compared with 1996 in 2000, the number of students enrolled in key undergraduate courses in the whole region increased from 85 to 184, from 185 to 54 1 person above provincial undergraduate courses, and from 3 15 to 829 above provincial specialist courses.
Geomorphology of Baiyun District:
Baiyun District is high in the north and northeast, and low in the west and south. Roughly bounded by Guangcong fault zone and Shougouling fault zone, it is adjacent to Guangcong fault zone in the east and Shougouling fault zone in the north, and it is a Baiyun Mountain-Luogang hilly region, which is dotted with intermountain alluvial plains, such as Luogang Cave alluvial by Nangang River and Suifeng and Xingfeng small basins alluvial by Jinkeng River.
Alluvial materials of Baimi Cave in Liangtiankeng and Jiufo Cave in Fengweikeng, etc. Starting from the west of the fault, there are mainly Liuxihe alluvial plain and Pearl River Delta plain. The north and northeast are dominated by low mountains, with deep valleys and steep slopes. The bedrock is hard massive metamorphic rock and granite.
On the edge of low mountains, such as the east side of Xinguangcong Highway and the south side of Dayuan Highway, there are a series of hills, whose bedrock is medium-coarse grained granite with weak weathering resistance, so the top of the mountain is round and the hillside is gentle. On the southern edge of the hilly area, along the strike of Shougouling fault, there is a banded platform, starting from Wangshengtang in the west and connecting Zoumagang and Guihuagang.