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18 Cards in this Set

  • Front
  • Back

4 parts of soil

1- minerals


2- bacteria and organic material


3- air


4- moisture

minerals

- join soil when the rock is broken down


- many needed by plants

bacteria and organic material

- dead plants + animals decomposed by material


- nutrients released


- enhance soil

air

- Decaying materials allow for air pockets


- Air spaces created by insects

moisture

- Dissolves nutrients into soil

- Helps decay organic materials

continental drift evidence

- Alfred Wegener


1. Jigsawfit between south America and Africa2. Fossilsof same plants and animals on south America and Africa


3. Mountainsof similar ages in north America and Europe


4. Icesheets covered south Africa, India, Australia, and south America

calcification

- In drier climates

- Water in the topsoil evaporates


- Water drawn up from below to replace it


- Minerals carried up with water Process is called capillary action


- Water reaches surface, and evaporates

leaching

- Occurs in wet climates or over watering

- Water moves downward through the soil


- Carries nutrients to the parent material


- Soil leached of nutrients


- Plants need nutrients to grow

alpine tree line

- Highest elevation trees can grow on mountains

- Too cold, snow cover


- Steep slopes= thin soil

arctic tree line

- Trees cannot grow to the north

- Cold temperature, poor soil


- Permafrost prevents long roots

drunken forest

muskeg near churchill MB

natural vegetation

- plants that grow without human interference


- vegetation determined by climate and soil

permafrost

- permanent layer of frozen ground below active layer


- snow above the active layer melts

soil profile

different layers in the soil

top soil

- contains humus where plants grow

sub soil

- 2nd layer


- minerals and organics

parent material

- bottom mineral materials


- top soil added through organic breakdown


- formation is very slow

climatic graphs

Shows relationshipsbetween temp + precipitation month by month