Upload
elfreda-stephens
View
215
Download
1
Embed Size (px)
Citation preview
A mineral is a… ADD HERE
NATURAL
Minerals are created by the… ADD HERE
INORGANIC
Minerals are not made by living things or are composed of living
things.
CRYSTALLINE
The arrangement of atoms within a mineral creates a crystalline structure… ADD
HERE
CHEMICAL COMPOSITION
Minerals are composed of one element or many elements… ADD HERE
Chemical Composition of Minerals
ADD HERE
Ex: Sulfur = S
Some minerals are composed of a combination of
elements… ADD HERE
Ex: Fluorite = CaF2
(combination of calcium and fluorine)RT = Pg. 16
Crystalline Structure of Minerals
The atoms with a mineral are arranged and bonded in a specific way creating the crystalline structure of the
mineral.
The crystalline structure of a mineral helps to determine that mineral’s physical and chemical properties – such as
hardness and cleavage.
The majority of the Earth’s crust (by mass and volume) is made up of the elements oxygen and
silicon. The “silicon-oxygen tetrahedron” is the basic
building block of many minerals.The arrangement of silicon-oxygen
tetrahedrons… ADD HERE
Rock vs. MineralA rock is a… ADD HERE
All minerals are rocks, but not all rocks are minerals.
Most rocks are composed of one or more minerals. Some rocks are composed of
glassy or organic materials
COAL
Coal is composed of the… ADD HERE
Minerals are…ADD HERE
OBSIDIAN
Obsidian is volcanic glass that is formed by heated rock being cooled very quickly. Glass has a
noncrystalline atomic structure.
ADD HERE…
Mineral Properties and Identification The best method for
mineral identification is through the use of X-ray
diffraction.
A beam of X-rays passing through a
mineral sample will diffract leaving a unique
“x-ray pattern” on photographic film.
Each mineral has its own unique diffraction
pattern.
Minerals have a unique set of physical and chemical properties that reflect its internal arrangement of atoms.
When in the field, scientist will use other methods to identify minerals.
Mineral Properties and Identification Color
The color of a mineral can be used for identification in some cases. Many times minerals will change due to impurities found within the rock
or mineral.
Color is NOT a reliable mineral property used in identification
SULFURSulfur is well known for
its yellow color.
QUARTZAll three samples are of
the same mineral. In this case color would not be useful tool in mineral
identification.
Mineral Properties and Identification Streak
The residue of a mineral… ADD HERE
The streak color does not always match the color of the mineral.
The streak of a mineral is more consistent than the
color of a mineral and, therefore, is a more
reliable test for mineral identification.
HEMATITEHematite is a silver colored mineral.
When scratched on a porcelain plate, its streak is reddish-brown.
Mineral Properties and Identification Luster
ADD HERE…
Minerals may have… ADD HERE
A mineral with a metallic luster shines like a metallic surface (Ex: clean steel pot).
Most minerals have a nonmetallic luster.
PYRITEPyrite has a metallic luster and
shines like a metallic surface in the light.
OLIVINEOlivine does not shine like a metallic
surface in the light. It has a nonmetallic luster.
Mineral Properties and Identification Hardness
ADD HERE…
Moh’s Hardness Scale is a tool used by scientists to determine the hardness of a mineral. Scientists can determine whether an unknown mineral can “scratch” or be “scratched” by known common materials.
This will help a scientist determine the hardness of an unknown mineral.
Gypsum has a hardness of 2 and calcite has a harness of 3. A
fingernail has a hardness of 2.5. A fingernail can “scratch”
gypsum and “be scratched” by calcite.
Mineral Properties and Identification Cleavage
The tendency of a mineral… ADD HERE
Zones of weakness found within a mineral relate to the crystalline structure of
the mineral.
Sometimes zones of weakness can be seen as
smooth sides with a luster.
Minerals that lack zones of weakness… ADD HERE
MUSCOVITE MICA
GALENA
CLEAVAGE:Zones of weakness
FRACTURE:Uneven brake