The radial stream drainage pattern is the most common type of drainage pattern.
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Q10: Internal drainage basins sometimes have highly salty
Q11: Streams in undeveloped areas experience sudden spikes
Q12: There are two main types of flooding:
Q13: Geologic uplift gives streams more energy to
Q14: Waterfalls slowly migrate downstream through erosion.
Q16: Drainage basins are usually small and geographically
Q17: Natural levees are built up only during
Q18: Stream deposits are often sorted by size.
Q19: Dams and reservoirs reduce peak discharge amounts
Q20: Meanders only develop in low-gradient streams.
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