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Qaagi - Book of Why

Causes

Effects

In addition , waves carry pieces of pebble , stone , and sandcauseweathering in rocks

In addition , waves probability based option trading pieces of pebble , stone , and sandcauseweathering in rocks

Fragmental materialoriginatesfrom weathering of rocks and is transported by

Fragmentary materialoriginatesfrom weathering of rocks and is transported by

to showcausesweathering in rocks

surfaces sediment - fragmented materialoriginatesfrom weathering of rocks and is transported by

rustcausesweathering in rocks

Sediment – Solid particles or masses of particlesoriginatefrom the weathering of rocks that are transported

several factorscausingweathering in rocks

three thingscauseweathering in rocks

them to release minerals , such as phosphorus , into the soil and watercausesthem to release minerals , such as phosphorus , into the soil and water

REE fractionation during granite weatheringMobility of REE(passive) is influencedREE fractionation during granite weatheringMobility of REE

nutrientscontributesnutrients

silt and clay ... and microbes and fungi also erode rock material into ever tinier bitscan createsilt and clay ... and microbes and fungi also erode rock material into ever tinier bits

to partial transfer of potassium to water ... but this is rapidly absorbed by organisms and claysleadsto partial transfer of potassium to water ... but this is rapidly absorbed by organisms and clays

in the formation of clay minerals such as kaolinite and smectiteresultedin the formation of clay minerals such as kaolinite and smectite

the arsenic - bound compounds to be washed into the rivers , only to be deposited in lowland basins and deltas , which is where most of the contamination is observedcausesthe arsenic - bound compounds to be washed into the rivers , only to be deposited in lowland basins and deltas , which is where most of the contamination is observed

jolts in northern Sumatra Bandungcausesjolts in northern Sumatra Bandung

negative feedbacks(passive) caused bynegative feedbacks

a negative feedback on atmospheric CO 2 amount [ 3 ... as discussed in section 3 ... but this feedback is too slow to alleviate climate change of concern to humanitycausesa negative feedback on atmospheric CO 2 amount [ 3 ... as discussed in section 3 ... but this feedback is too slow to alleviate climate change of concern to humanity

natural spaces(passive) created bynatural spaces

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