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CHAPTER 13 SURFACE WATER. 13.1 STREAMS AND RIVERS. WATER CYCLE. RIVER SYSTEMS. A RIVER AND ALL IT’S TRIBUTARIES TRIBUTARIES – SMALLER STREAMS THAT RUN INTO THE MAIN RIVER – AND CARRY ERODED ROCK – SEDIMENTFOR RS ACCOUNT FOR MOST EROSION ON EARTH’S SURFACE. DRAINAGE BASIN / WATERSHEDS.
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CHAPTER 13 SURFACE WATER 13.1 STREAMS AND RIVERS
RIVER SYSTEMS • A RIVER AND ALL IT’S TRIBUTARIES • TRIBUTARIES – SMALLER STREAMS THAT RUN INTO THE MAIN RIVER – AND CARRY ERODED ROCK – SEDIMENTFOR • RS ACCOUNT FOR MOST EROSION ON EARTH’S SURFACE
DRAINAGE BASIN / WATERSHEDS • ALL THE LAND THAT DRAINS INTO THE RIVER • SEPERATED BY DIVIDES
CONTINENTAL DIVIDE • RUNS THROUGH ROCKY MOUNTAINS • RAIN FALLING TO THE • WEST FLOWS TO PACIFIC • EAST FLOWS TO ATLANTIC
MISSISSIPPI RIVER WATERSHED • LARGEST SINGLE DRAINAGE BASIN IN U.S. – 4.76 MILLION km2 • WEST DIVIDE= CONTINENTAL DIVIDE • EAST DIVIDE = APPALACHAIN MTNS
MISSISSIPPI RIVER WATERSHED DUBOIS
PA DRAINAGE BASIN SUSQUEHANNA VALLEY WATERSHED CHESAPEAKE BAY WATERSHED
CHARACTERISTICS OF STREAMS AND RIVERS • ABILITY OF STREAMS AND RIVERS TO ERODE, TRANSPORT AND DEPOSIT SEDIMENT IS AFFECTED BY MANY FACTORS • FACTORS INCLUDE: • VELOCITY OF WATER • GRADIENT OF STREAM • DISCHARGE • SHAPE OF CHANNEL
STREAM VELOCITY • DISTANCE WATER TRAVELS IN GIVEN AMOUNT OF TIME • FACTORS AFFECTING SPEED: • STEEPNESS OF SLOPE • AMOUNT OF WATER • THE SHAPE OF STREAM
GRADIENT – STEEPNESS OF SLOPE • VARIES • AT SOURCE – LARGE • AT SEA LEVEL - SMALL SOURCE LARGE SMALL Gentle
DISCHARGE • NOT CONSTANT • GENERALLY INCREASE DOWNSTREAM • TRIBUTARIES ADD MORE WATER • DESERTS DECREASE • YEARLY VARIATION • SPRING MELTS – VELOCITY = MAYBE FLOODING = DISCHARGE
CHANNEL • THE PATH THROUGH WHICH WATER FLOWS • SIZE SHAPE AFFECT VELOCITY SLOW MORESURFACE AREA FAST LESS SA
HOMEWORK • READ 280 – 282 • DO 13.1 RSG • AND 1,2,4,5 PG 282