Mineral Crystals and Major Mineral Groups Section 5.2
Slide 2
MI-2 Performance Tasks 2. Describe the factors that determine
how minerals grow. 3. Distinguish between minerals by the six basic
mineral shapes. 1.Define and describe crystal structure.
Slide 3
How did these mineral crystals grow to be so large?
Slide 4
Slide 5
MexicoMexico's Cueva de los Cristales (Cave of Crystals)
contains some of the world's largest known natural
crystalstranslucent beams of gypsum as long as 36 feet (11 meters).
Volcanic activity that began about 26 million years ago created
Naica mountain and filled it with high-temperature anhydrite
gypsum. When magma underneath the mountain cooled and the
temperature dropped, the anhydrite began to dissolve and for
millions of years have been deposited in the caves in the form of
huge selenite gypsum crystals.
Slide 6
Factors that determine crystal size: 1.Time 2.Space
3.Temperature 4.Pressure 5.Concentration Largest uncut diamond
found in the Letseng Mine in southern Africa. A near-flawless white
gem weighing nearly 500 carats. It was discovered on Sept. 8, 2008
It weighs 478 carats, with very few inclusions and of outstanding
color and clarity.
Slide 7
1. TIME and mineral formation The RATE at which the molten
magma cools determines the crystal size.
Slide 8
If the magma cools at a s-l-o-w rate then the crystals will. *
(example: granite) be LARGE and well-formed #44
Slide 9
If the magma cools at a fast rate, quickly, then the crystals
will. *example: obsidian cools instantly so it has no crystal
structure, but a glass-like structure be small / microscopic / not
well-formed / none
Slide 10
Summarize in a sentence: So. To grow the biggest, best
synthetic diamond crystal, you would. time, space, cooling rate
(temperature) pressure concentration
Slide 11
It takes Gemesis Diamond Co. four days to grow a diamond of an
average 2.5 carats. The process begins by placing a microscopic
diamond grain into a 4,000-pound machine about the size of a
kitchen oven. Under hundreds of thousands of pounds of pressure and
at temperatures as high as 2,700 F, the nugget grows, one atom at a
time. It uses about 20 kilowatt-hours per carat, The Gemesis
process mimics a diamond's development deep underground. Apollo
Diamond, based near Boston, takes a different tack, imitating the
way diamonds are made in space. Through chemical vapor deposition,
Apollo's process pumps gas into a chamber that essentially rains
carbon and forms a diamond nugget from a "seed" within two to four
weeks time. http://www.youtube.com/watch?v=48NoIICJ2CQ February 14,
2007 3:19 PM PST Synthetic diamonds still a rough cut By Elsa
Wenzel Staff Writer, CNET NewsElsa Wenzel
Slide 12
Classzone Internet Investigation ES0506 How Do Crystals Grow?
2. Space 3. Temperature 4. Pressure 5. Concentration
http://www.classzone.com/books/earth_science/terc/content/investigations/es05
06/es0506page01.cfm?chapter_no=05
Slide 13
Part A: Make and define a crystal The regular repeating
dendrite (branching) pattern of crystals
Slide 14
Part B Concentration and Crystal Formation Dead Sea: salinity
level 33.7% (8.6 times saltier than any ocean)
Slide 15
Part C Space and Crystal Size Classzone.com activity
ES0506
Slide 16
Part D The effect of the rate of crystal cooling on crystal
size and formation Phenyl salicylate (salol): What happens to the
crystal size formation when it cools slowly? When it cools
quickly?
Slide 17
________: clear, whitish, transparent _______________: pink,
salmon-colored ___________________: black, gray, dull
________________: black, shiny quartz Feldspar (potassium)
Hornblende (amphibole ) Mica - biotite Granite contains three main
minerals. Part E Cooling Rate and the Crystal Size of Granite
Slide 18
Each mineral melts / crystallizes at its own temperature
between 1200C and 500C Hornblende
Slide 19
Rank the order in which the minerals in granite will
crystallize. First to cool and crystallize ___________ 2 nd to
crystallize ___________________ 3 rd to crystallize
___________________ Last to crystallize _________________
Hornblende (amphibole) Feldspar (potassium) - pink quartz So...
Quartz is the LAST to crystallize, so it is usually shapeless.
Biotite mica
Slide 20
Slide 21
Part F1 Potassium nitrate crystals Salt crystals Borax
crystals
Slide 22
Crystal Shapes (page 99) Crystal: the orderly arrangement of
the ions, atoms and molecules determines the shape of each minerals
crystals.
Slide 23
Part F2: Crystal Shape Activity In your note book: Paper model
letter Crystal name Example Mineral name Tray sample 1 2 3 4 5 6
Use table on page 99 in your text book F3 : Look at the crystal
samples in the trays under the stereoscopes. Match them to the
crystal models. A C F D B E Cubic Tetragonal Hexagonal Orthorhombic
Monoclinic triclinic Halite (Salt) Zircon Emerald Topaz Sulfur
Gypsum Mica turquoise
Slide 24
Minerals as Gems
Slide 25
Mineral Gemstones A gemstone is defined as Whats the difference
between precious and semi-precious stones? What does it mean?
Slide 26
Tumbled Gems Stones Gems are valued for their reflective
properties due to the way they cut (facets).
Slide 27
Rough, uncut vs. polished unpolished Malachite Turquoise Opal
topaz emerald
Slide 28
Our State Mineral Top 5 facts 1.What is the name of our state
mineral? 2.What color is our state mineral? 3. What elements, the
chemical formula 4. Mineral characteristics 5. How its formed 6. It
is found where in Illinois. 7 Value and uses as a mineral resource
What group of minerals does it belong to
Slide 29
State Mineral Quiz 1.What is the name of our state mineral?
2.What two elements make up our state mineral? 3.It was formed by
which method: magma process, heat/pressure,
evaporation/precipitation 4. Where in the state is/was it mined? 5.
What is an unusual characteristic of it?
Slide 30
5-4-3-2-1 Home work! List the 5 characteristics of a mineral
Describe 4 factors and how they effect crystal size Describe 3 ways
that mineral form Diagram 2 polymorph forms of carbon Name the 1
most abundant mineral group in the earths crust