Drainage networks develop in response to specific rock structures and surface slopes. How do the following drainage pattern types match with their primary geological controls?
- Dendritic patternUniform lithology with flat-lying, homogeneous rock strata
- Radial patternConical hills, volcanic domes, or central high peaks
- Trellis patternAlternating parallel belts of hard and soft folded rocks
- Centripetal patternInward-sloping interior basins or central depressions
Cevap
Dendritic pattern pairs with uniform lithology and flat-lying strata; Radial pattern pairs with volcanic domes or central peaks; Trellis pattern pairs with alternating bands of hard and soft folded rocks; Centripetal pattern pairs with inward-sloping interior basins.
Each drainage pattern reflects specific surface geology: dendritic networks form on uniform rocks with equal erosion resistance, radial networks diverge outward from central domes, trellis networks align with alternating bands of folded rocks, and centripetal networks converge inward toward central basins.
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Anahtar Kavram
Geological Controls on Drainage Patterns