River patterns - dendretic
Looks like a tree
tribituaries meet main river at acute angles
Gentle slopes w uniform rock types
River patterns - Trellis
Looks like an phone tower
Tribituaries meet river at 90 degree angles
Large river eroded downwards into softer rocl
Harder rock left elevated above it
River patterns - Radial
Tribituaries flow from a circle or oval shaped mountain.
Tribituaries flow out like wheel spokes
River patterns - Parallel
Rivers flow parallel + don’t join. Straight course separated by steep slopes
River patterns - Deranged
Disorganised + chotic tribituaries. Swamp or marsh
River basin - Source
Where a river begins, usually high ground
River basin - Tribituary
Small river that joins a bigger one
River basin - Confluence
The point where 2 or more rivers join together
River basin - Mouth
Where the river meets the sea
River basin - Course
Path a river flows along
River basin - Watershed
Highland area that separates 1 drainage basin from another
River basin - Estuary
Tidal part of the river mouth, where the river water meets the sea
River erosion - hydraulic action
Water hits off riverbed and bank, breaks off rocks
River erosion - Abrasion
Eroded materials hit off the bed and banks, loosening other rocks + soil
River erosion -Attrition
Rocks and pebbles hit off eachother gradually wearing eachother down
River erosion -Solution
Soluble rock particles disaloved by weak acids in the water
River transportation - Suspension
Particles lifted off the riverbed + carried
River transportation - Saltation
Pebbles + stones bounced off the riverbed
River transportation - Traction
Heavy rocks rolled along the riverbed
River deposition causes
Loss of velocity - old age stage + dams
Loses volume - distributaries, heat + irrigation
Increased load - heavy rainfall = more erosion = more load
Waterfalls - Eg
Powerscourt, Co. Wicklow
Waterfalls - Description
Vedrtical drop in a riverbed formed in the youthful stage due to vertical erosion
Waterfalls - Explanation
Hard rock lies (granite) upstream of soft rock (limestone)
Differential erosion from hydraulic action - soft rock eroded
Hydraulic action + abrasion create plungepool below where soft rock was eroded
Rock undercut by solution creating an overhand
The overhang eventually collapses causing upstream erosion
Meanders - eg
River Liffey