What was the aim of our river fieldwork?
To investigate how river channel characteristics (width, depth, velocity) change downstream at Carding Mill Valley.
What hypothesis did we test?
That the river would become wider, deeper, and faster flowing downstream.
Why was Carding Mill Valley a suitable location?
It is safe, accessible, and shows clear upstream–downstream changes in river characteristics.
How did we measure river width?
We stretched a tape measure across the channel from bank to bank.
How did we measure river depth?
We took multiple depth readings at equal intervals across the channel using a meter ruler.
How did we measure river velocity?
We timed a floating object (e.g., cork) traveling a set distance downstream.
Why might our velocity data not have been accurate?
The float often got stuck on rocks in the uneven riverbed, causing slower readings.
What trend did we find for river width downstream?
Width increased downstream.
What trend did we find for river depth downstream?
Depth increased downstream.
What trend did we find for river velocity downstream?
Velocity generally increased downstream.
Which geographical theory supports our findings?
The Bradshaw Model (predicts increased width, depth, and velocity downstream).
What physical process explains increasing depth downstream?
Vertical erosion deepens the channel as water energy increases.
What physical process explains increasing width downstream?
Lateral erosion wears away the banks as discharge increases.
Name one risk during fieldwork.
Slipping on wet rocks in the river.
How was the slipping risk reduced?
By wearing sturdy shoes with good grip and entering the river slowly.
How could we improve reliability?
Repeat each measurement and calculate an average.
How could we improve accuracy?
Use a flow meter instead of a float to measure velocity.
Why might our conclusions not be fully valid?
We only collected data on one day and at ten sites, so results may not show typical conditions.