Earth Flashcards
What are rocks made of
Minerals
What are minerals
Naturally occurring Distinct chemical composition Distinct physical properties Crystalline structure Inorganic (not living)
What is a gemstone
Usually a mineral, one that formed crystals then cut and polished to be made jewelry
How do you tell what a mineral is
Lustre Hardness Cleavage/Fracture Streak Colour
Lustre
Shiny or dull
Metallic or non-metallic
Colour
One best describes the minerals appearance
Streak
The colour of the powder of the mineral, can be a different colour.
(Making a streak with the mineral on a white, dull surface like paper)
Cleavage or fracture
The way the mineral breaks apart
Fracture is rough and jagged break
Cleavage is a smooth flat surface broken
Hardness
Hard or soft
Use teh Moh’s hardness scale (scratch test)
1 is the softest and 10 is the hardest
Igneous rocks
formed by melting and cooling of lava or magma Contain crystals Intrusive rocks form below the surface Extrusive rocks form above the surface Granite, basalt, gabbre
Sedimentary rocks
Formed when sediments (small bits) settle and form layers
Often contain fossils
Sediments are compacted and cemented together
Sandstone, limestone, conglomerate
Metamorphic rocks
Formed below earths surface
Heat and pressure cause existing rock to transform
Marble, Quartzite, Slate
Erosion
Movement of soil, rocks and minerals from one place to another
Gradual such as glaciers
Sudden change such as flash floods or earthquakes
What are the 4 agents of erosion
- Gravity
- Glaciers
- Wind
- Moving water
Weathering
The breaking down of rocks into smaller rocks and sediment
The 3 types of weathering
- Mechanical
- Chemical
- Biological
Mechanical weathering
Caused by: Gravity Temperature change Wind Water
Examples of mechanical weathering
Rock slides
Frost wedging
Rivers
Chemical weathering
Caused by chemical reactions
Examples of chemical weathering
Acid rain from pollution
Rust
Biological weathering
Caused by living things
Can be Mechanical OR Chemical
Examples of biological weathering
Tree roots in a sidewalk
Lichen or rocks
Sedimentation
the opposite of weathering and erosion because it’s the process of soil being deposited resulting in teh formation of sedimentary rock
Mold
Forms when an organism is buried in sediment.
Decays over time leaving an imprint of the organism behind
Like a cake pan
Cast
Can a form after a mold fossil
Minerals, sediments and water fill it
Over time water evaporates cementing the sediments leaving behind a cast
If a mold is a cake pan a cast is the cake
Carbon film
All living things contain carbon.
An organism that dies and is buried will break down until all is left is carbon
like a stamp left
Traces fossil
A fossil that provides evidence that an organism lived rather than part of the organism itself
footprints, bite marks, tunnels, poop
Preserved remains
Sometimes fossil form leaving the organism very close to their living state, they can form in:
- Tar
- Amber
- Ice
Petrified fossils
Forms as an organism decays being replaced with minerals and sediment.
Water will seep in while an organism weathers
evaporates leaving the dead organism in the place it died
What are the 4 timescale geologically
- Eons
- Eras
- Periods
- Epochs
Geologic timescale
A timescale over the 4.6 billion years of earth broken down into Eons Eras Periods Epochs
Stratigraphy
The study of rock layers and what may be found within them (fossils)
What are the 4 eras
- Precambrian
- Paleozoic
- Mesozoic
- Cenozoic
Principle of Superstition
Oldest layers are at the bottom Youngest layers are at the top Layers are called Strata Layers from oldest to youngest: Shale Sandstone Shale Lava flow Limestone
Strata
Layers in rock
Relative age
Looking at which strata it’s in to determine how old
If there is a crack goes through the layer it must’ve happened
Index fossils
Used to determine the relative age of layers
Radiometric dating
Scientists look at the half life of an enemy in the rock
By looking at how much is left they can tell how long that rock has been there for
Half-life
The amount of time it takes for half of a radioactive material to turn into another material
Radiocarbon dating
A form of radio metric dating that scientist look at the half-life of carbon-14
C-14 has a short half-life
Used to measure fossils/living things
After 50 000 years there’s not enough C-14 to accurately measure