• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/13

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

13 Cards in this Set

  • Front
  • Back

F O O T P R I N T S

By Halle Cambey

ROCKS

- Come from Earth's crust


- Earth's crust is the thin layer of the Earth


- About 30km thick on lan and 8km thick under the sea


- three types of rocks: ingeous, metamophic, sedimentary

Sedimentary rocks

- formed from minerals that are left behind when water evaorates


- often have layers showing the deposition of sediments at different time periods.


- made of lots of grains


- often have fossils trapped within them

Metamorphic Rocks

- formed by being squeezed an twisted together


sedimentary rocks are turned into metamorphic rocks by the extreme pressure

Igneous Rocks

- formed when the magma cools and solidifies


- contains interlocking crystals that are held together very strongly

TEMPERATURE VS CRYSTAL SIZE

- crystal growth depends on lots of different variables


- temperature has a direct impact on the size and the speed which crystals grow


- the warmer/ higher the temerature, the more rapid te growth of the crystal but the smaller it would be.


- the lower the temperature, the larger the crystal will grow.

WEATHERING

-Physical Weathering: is when rocks break down of rock by water and temperature



- Chemical Weathering: break down of rocks caused by chemicals and the water in the air.

EROSION

- the movement of soil and weathered rocks from one place to another through means such as water, wind, humans, ice. etc



- DEPOSITION: is the layering down of eroded material in a different place.

MODELS IN SCIENCE

- models hel us to visualise and understan the princils of science and scientific theories

THE ROCK CYCLE

1. Igneous rocks


2. Weathering, erosion and deposition


3. heat and pressure


4. sedimentary rocks


5. heat and pressure


6. metamorphic rocks


7. heating


8. magma


9. cooling

FOSSILS

- preserved remains or traces from pervious life


- to produce fossils, the living organism bust be buried


- formed by small fragments are transported to the sea, they sink and form a sediment


- small animals become trapped within the sediment


- over millions of years, the pressure of layers above, cement the sediment together

GEOLOGICAL TIMESCALE

- universe began 13.7 million years ago


- solar system took shape 4.57 billion years ago


- Earth formed 4.54 billion years ago


-moon formed 4.5 billion years ago


- first cells came 3.8 billion years ago


- cambrian explosion 542 million years ago


- evolution of humans 200,000 years ago

GRAHS, TIMELINES AND DICHOTOMOUS KEYS

- information used to classify organisms


- a graphical representation of a period of time, on which important events are marked.