WEEK 8 - Rivers Flashcards
What Do Streams in the Earth System Do?
- Streams carry water across land and connect it to the sea.
- They move excess water (from rain) that doesn’t soak into the ground or evaporate.
- Act as major water flow pathways on Earth’s surface.
What is a Stream?
- A stream is flowing water that moves downhill in a channel.
- It carries rock particles and dissolved ions (from weathered rocks).
Why Are Streams Important?
- Move water from land to sea
- Erode and move sediment (helps form sedimentary rocks)
- Carry dissolved minerals to oceans (why oceans are salty)
- Provide water and are used for transportation
→ Many cities are built along streams
Origin of Streams – Where Does Rainwater Go?
- Evaporate into the air
- Soak into the ground (becomes groundwater)
- Stay on the surface as runoff → flows into streams
How Runoff Becomes a Stream
- Runoff first spreads out in a thin layer = sheetflow
- Then it gathers into small channels = rills
- These rills may grow into larger streams over time
How Streams Grow Larger
- Rills merge into larger, more permanent stream channels
- These streams become tributaries of bigger rivers
- A river is just a stream with multiple tributaries
What Are The Stream Characteristics?
- Ability to downcut
- Gradient
- Load
- Stream Flow
- Channels
- Valleys
Stream Characteristics – Ability to Downcut
- Streams erode downward to reach base level (sea level)
- The higher the elevation above sea level, the faster the downcutting
- Erosion is strongest at the headwaters (highest points)
Stream Characteristics – Gradient
- Gradient = the slope of the stream
- Higher gradient at the headwaters (upper part of stream)
- Lower gradient near the mouth (where the stream meets the sea)
Stream Characteristics – Load (Three Types)
- Stream Load
- Bedload
- Suspend Load
What is Stream Load? (Load)
- How streams carry sediment
What is Bedload? (Load)
- Large/dense particles
- Move by tumbling or saltation (bouncing)
- Stay mostly on the bed of the stream
What is Suspended Load? (Load)
- Small/light particles
- Stay suspended in the water (small and light particles (e.g., dirt, sand, clay) float in the water, carried by the flow, instead of sinking to the bottom)
What do Bedload and Suspended Load have in common?
Both decrease in size as the stream moves downstream (away from sediment source).
Stream Characteristic - River Flow (Two Types)
- Turbulent Flow
- Laminar Flow
What is Turbulent Flow? (River Flow)
- Occurs near the bottom and sides of the stream.
- Water moves in swirling, chaotic patterns (called eddies).
What is Laminar Flow? (River Flow))
- Occurs in areas away from turbulence.
- Water flows in smooth, straight lines.
Common Misconception: River Speed
- In The House at Pooh Corner, it says streams are faster near their source and slower farther down.
- But actually, rivers can flow faster downstream because they get more water from other streams, even though the slope may be gentler.
Stream Characteristics - Channels (Two Types)
- Headwaters
- Lower Course
What is Headwaters? (Stream Channel)
- Small, shallow channels
- Coarse bedload (larger particles)
- Turbulent flow (swirling water)
- Low overall velocity (drag affects most of the water)
What is Lower Course? (Stream Channel)
- Large, deep, wide channels
- Fine bedload (smaller particles)
- Laminar flow (smooth water)
- High overall velocity (drag near the stream bed)
Stream Characteristics - Valleys
- River channels are surrounded by valleys.
- Valleys form when streams wear away the river banks.
- The weakened banks crumble and fall into the river.
- This material becomes sediment the river carries.
Valleys at Headwaters
- High above base level.
- Tend to be deep and V-shaped.
- Rapid downcutting creates this shape.
- No strong meandering (snake like) pattern
Valleys in Lower Parts of Stream
- Close to base level.
- Tend to be broad due to less downcutting.
- More lateral movement (sideways erosion).
- Meandering pattern more noticeable.