九华山地区受新生代断块活动影响，沿九华山逆断裂带，上盘隆升为山地，形成南北绵延30余公里的九华山大型花岗岩石岭群峰；下盘下降成宽阔绵延起伏的丘陵、盆地。从九华山地质公园游客中心到花台顶峰的6km直线距离，完成了从盆地（平均海拔30m）到丘陵（平均海拔270m）再到山地山峰（平均海拔1000m以上）的地貌变化，即为“峰-丘-盆”的壮美景观。 Jiuhuashan area was impacted by Cenozoic fault-block movement. And hanging side of Jiuhuashan reverse fault zone was uplifted to become mountain land which is Jiuhuashan large-scaled granite peaks and ridges stretching 30km long in south-and-north direction. And heading side declined to become broad and gently rolling hill and basin. Within 6 km straight distance from Tourist Service Center of Jiuhuashan Geopark to Tianhua Peak., landform changes from basin (average altitude: 30m) to hill (average altitude: 270m) and to peak (average altitude: over 1000m), namely a spectacular peak-hill-basin landscape.