Mapa mental
the rivER system,,

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the rivER system,,
waterfalls,,, nice ive never rly seen one lol
- gues what. coMMon sense time
- it's a sudDEn fall of water. it's a fALL OF WATER. WATER faLL. whAt did u thiNK IT WAS
- what's not common sense is?? how it's formed :0
- river flows from resistant 2 less resistant. ah, that makes sense!!
- so the downstream not resistant rocks = !! eroded faster !! omg waterfall commENCE
- but w/ ths said, use the keywords GRADIEnt and dIFFERENTIAL EROSION!!!!!!!
- so the downstream not resistant rocks = !! eroded faster !! omg waterfall commENCE
- river flows from resistant 2 less resistant. ah, that makes sense!!
- pLUnge pools, too !!
- ... haha water PLUNGEs against the rocks below the waterfall,
- but alas, it's not that simple . this depression is deepened & enlarged by the HYDRAULIC ACTION of the plunging water !! and also, the swirling of water there, causing aBRASIOn.
- there u have it! a plunge pool
- but alas, it's not that simple . this depression is deepened & enlarged by the HYDRAULIC ACTION of the plunging water !! and also, the swirling of water there, causing aBRASIOn.
- ... haha water PLUNGEs against the rocks below the waterfall,
- annotation coming
- okay so undercutting = gorge
- the overhang str8 up collapses :00
- and then the plungepool !! yaY
- the overhang str8 up collapses :00
- okay so undercutting = gorge
- gues what. coMMon sense time
blue, to represent wATER
meanders
- bends in a river as sinuosity increases
- usually occur in rivers w coarser load,,
- they lied. they said we aren't tested on pools & riffles, but its related so listen up
- carisse.. what r pools nd riffles
- pools r deeper parts of the river where fine sediments like silt ! r deposited
- riffles r shallow !! where coarser stuff like pebbles r deposited
- um.. hoW?? u make 0 sense
- riffles slow down velocity before it picks up again!! neat
- so like,, alternating velocity, different levels of erosion = meander s!
- riffles slow down velocity before it picks up again!! neat
- carisse.. what r pools nd riffles
- water tends to flow faster around the bends on the oUTER side, more erosion!1
- then this eroded stuff slides down, forms a river cliff ,,, the cliff is concave shaped !! so conCAVE BANK, outsiDE
- as for the inner banks, water is slower, more deposition!!
- deposits have this gentle slip off slope,, inner bank = convex bank
- bends in a river as sinuosity increases
oxbow lakes
- gdi. they should call it a horseshoe lake. it's horseshoe shaPED
- formed after meanders!1 lateral erosion & undercutting occur on the concave bank, deposition on convex
- the continuous erosion / deposition make the convex and concave bank get closer,, basically a v pronounced meander
- yEs ! the narrow neck of land is finally cut through, either by lateral erosion of 2 concave banks or the v strong currents of a flood
- the continuous erosion / deposition make the convex and concave bank get closer,, basically a v pronounced meander
- formed after meanders!1 lateral erosion & undercutting occur on the concave bank, deposition on convex
- gdi. they should call it a horseshoe lake. it's horseshoe shaPED
levees
- ok so like. when it floods !! we got a problem
- but we have levees!1 niCE
- basically, levees block the water from overflowing and going where we don't want it to go.
- they're naturally made of earth!! like the natural movement of water pushes the sediments to the side of the river
- ok so like. when it floods !! we got a problem
floodplaiNS
- are like, plains which hold the excess water when there;s a flood!
- they hodl the excess water that gets past the levees to prevent furTHEr flooding,,,
- okay here's some annotating for the rly small picture
- the green part is the flood plain. when the river floods, that's where the flooded water goes !!!!!!!
transportation
- foUR TYPEs
- (1) SOLUTION
- minerals r dissolved in the water and carried along as a solution!!
- (2) SUSPENSIOn
- rEEaaaly fine particles are brought along in the water !!
- (3) SAltation
- small pebbles & stones bounced along the river bed !! ah cute
- (4) TRACTIOn
- hUUuuge ass boulders / rocks are bounced bOUcned along the river bed :))
- (1) SOLUTION
- foUR TYPEs
eroSION!!!!
- FOUR TYPEs
- (1) HYDRAULIC ACTION
- the force of the river against the banks which causes air to be trapped in the cracks. the pressure weakens the banks and gradually wears it away
- (2) ABRASION
- rocks carried along by the river wear down the bed and banks !!
- (3) ATTRITION
- rocks being carried by the river smash tgt and break in2 smaller particles
- (4) soLUTION
- soluble particles are dissolved into the river,,, some acidic thing lmAO
- (1) HYDRAULIC ACTION
- FOUR TYPEs
u better know how 2 annotate
- oxbow lakes, levees, plunge pools & waterfalls
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- @ sophia::: this is mesy as hel
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- sympathy
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