The macrostructure of the landform of the North of Guangdong appearsas a net pattern.There are basins in the interiors of nets

mountainous regionsin the arrises of nets.The neotectonic movement in this area is chiefly charac-terized by extensive

spasmodic uplift.The uplift may arrive at 700 m or moresince Neogene Period

at 70m since a million years late.The vertical differentialerosion scales in distinct rock stratums and lithologies have arrived at n×100mmagnitudes.The forming of landform of North of Guongdongmainly is not thatmoving tectonics moved differentyl since a million years

but is that was erodedfor a long time on the basis of crustal movement befor a million years.The thesisis yet discussed the relationship between the groups of landform type andconditions of various resources and is raised proposals concerning utilization.