earth science day one

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Lab one • Part 1-the scientific method • Part 2-based on Hardness • (excell file)(Moh’s Scale • Part 3-based on cleavage • GOOD NEWS( most of the lab is done for You!! • Again-this is very boring but the exciting part is the concept of learning to classify items!!!

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Page 1: Earth science day one

Lab one

• Part 1-the scientific method• Part 2-based on Hardness • (excell file)(Moh’s Scale• Part 3-based on cleavage

• GOOD NEWS( most of the lab is done for You!!• Again-this is very boring but the exciting part is

the concept of learning to classify items!!!

Page 2: Earth science day one

Do not focus on the mineral itself

• Focus on the method

Page 3: Earth science day one

The whole lab

• Part 1-the scientific method• #1 on p.2 • #2 on p. 4-what is the difference between a

rock and a mineral• #4 on p. 8 –excell sheet• #5 p. 12• #6 –extra credit

Page 4: Earth science day one

Also . .

• Due sept. 16th –all properties will be used to identify rocks

• “how minerals effect every day life”• You must bring me the prelab assignment on

page 20-21 (INSULIN CRYSTAL GROWTH)

Page 5: Earth science day one

Lets start with p.2

• Part 1-the scientific method• “how did early geologists classify Earth

minerals?”• To simplify –in groups of 3-4-use one box• I will assign 6 geological samples to you• Please make a flow chart based on “what

stood out for you?”

Page 6: Earth science day one

Your group must pick one property , then . . another property and so forth!

Page 7: Earth science day one

The groups-please choose a name(

• Eratosthenes• James Hutton• Mary Anning• Friedrich Mohs• Alfred Wegener• Inge Lehmann• http://coolsciencelab.com/geologists.htm

Page 8: Earth science day one

Worksheet on page 2

Group Defining critieria for each groupSpecimens in Group

EEratosthenes

Jonathan,Trevis,Ana 5,10,4,10,9,3

. .

Page 9: Earth science day one

Eratosthenes-grade A+

• Jonathan,• Trevis,Ana

• 5,10,4,10,9 and 3

• Color=how many are brown?• 5 is brown, 4 is black, 10 is burgundy, 10a

clear, 9 white, 3 is black

Page 10: Earth science day one

Eratosthenes-high proficient talk-ready to press forward A+ work

• Texture• 5. softer than a glass , harder than a penny

pumice rock• 10. harder than glass and penny scoria rock• 4. harder than glass and penny obsideant rock• 10. softer than glass and penny• 9. softer than glass and penny and fingernail• 3. softer than glass and penny

Page 11: Earth science day one

Eratosthenes

• Went on to identify minerals to expert level of performance. Nice work “Eratosthenes”

Page 12: Earth science day one

James Hutton-did not present

• Stephanie • Amandy• Angie

• Rocks: 8,13,20,28,11 and 33• Color: 8 is grey, 13 is grey=20 is blk, 28 is grey• 11 is grey and blk, 33 is brown

Page 13: Earth science day one

Mary Anning-did not presentfossils

• Renee’,Mario, Arturo• 16,23,9,28,32,and 8• Color:• 16 is brown, 23 is beige, 9 is blk and white, 28

is green, 32 glass blk, and 8 is brownish grey• Texture:

Page 14: Earth science day one

James Hutton

• 3 grey minerals=luster

Page 15: Earth science day one

Friedrich Mohs-no comments- A+

• Marcy, Catherine, Chante’• 2, 15, 21, 5 and 20, 17

• Color : 2 is cloudy clear, 15 is clear, 21 is platinum, 5 is light grey with pink, 20 is transparent blue green, 17 is shimerry yellow gold

• Size: 2 large and heavy, 5 large nd heavy, 21 small, 17 large and light weight, 20 medium size, 15 large

• Hardeness: 2 hard as glass, 5 rough, 21 smooth as a penny, 15 hard as glass, 17 hard and rough, 20 harder than a penny softer than glass

Page 16: Earth science day one

Friedrich Mohs

• Next is shape:• This group had excellent presentation skills.• Demonstrated use of the scientific method.• All participants contributed, and no one was

isolated or unenvolved. Exceptional presentation guys.

Page 17: Earth science day one

Doppler Group-A+work

• Andrew, Danny

• 1, 6, 9, 16, 18, 20• Color: 1 is peach, 6 is black, 9 is white, 16 is

clear, 18 is black, 20 is green

• Texture-will finish this

Page 18: Earth science day one

Doppler Group-A+work

• This group went ahead to indentify hardness. They class would say they had sufficient knowledge of the scientific method which was the desired goal.

Page 19: Earth science day one

Alfred Wegener-did not present

• Andrea, Jermaine, Eunice, Troy

• 12, 20 , aa, ab, ac, ad• Color: 12 is black, 20 is black-all minerals• Shape: 12 and 20 rectangular(rhonbodal)• Aa and ab flat and rectangular• Ac and ad-chopped and screwed

Page 20: Earth science day one

Inge Lehmann-inner core-did not present

• Priscilla, Diane, Mary• 21, 20, 18 ,10 , 24 and 1

• Tetuxe: 21 is soft, 20 is rough, 18 is rough, 10 is really soft, 24 is not so rough, 1 is smooth

Page 21: Earth science day one

What is a justifiable property?

• Size• Shape• “is the rock clear, transparent, very dark?”• Texture-”feel smooth” • Etc.-this is calite• A rhombohedral• (60 degrees and • 120 degree angles)

Page 22: Earth science day one

Ladies( Like for diamonds

Page 23: Earth science day one

A sample flow chart

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For the credit for Part 1

• One person will have to present the flow chart to the class?

Page 25: Earth science day one

Part 2-based on Hardness

• What is hardness? Tourmaline • hardness : 7.0 - 7.5

Page 26: Earth science day one

http://academic.brooklyn.cuny.edu/geology/leveson/core/linksa/hardness_def.html

• "Hardness is a measure of how difficult or easy it is for a substance to be penetrated or scratched! For example, steel (like a steel nail) can scratch your fingernail, so steel is harder than fingernail!!"

Page 27: Earth science day one

Sample scale

• Finger nail• Penny • Glass

• First relative scale

Page 28: Earth science day one

Use the terminal in front of you . .

• http://library.thinkquest.org/J002289/mohs.html

Page 29: Earth science day one

Moh's Scale measures

• The Moh's Scale measures the relative hardness of various substances. It uses ten reference minerals. The hardness of a substance is determined by scratching it against a reference mineral. If it scratches that mineral, then it is of equal hardness or harder than that mineral, otherwise it is softer then that mineral. The picture below shows the minerals that are used on the Moh's Scale.

Page 30: Earth science day one

Quartz can scratch gypsum.

Page 31: Earth science day one

Can use this one as a comparison

Moh's Hardness ScaleHardness Mineral Description

1 Talc Fingernail scratches it easily.

2 Gypsum Fingernail scratches it.

3 Calcite Copper penny scratches it.

4 Fluorite Steel knife scratches it easily.

5 Apatite Steel knife scratches it.

6 Feldspar Steel knife does not scratch it easily, but scratches glass.

7 Quartz Hardest common mineral. It scratches steel and glass easily.

8 Topaz Harder than any common mineral.

9 Corundum It scratches Topaz.

10 Diamond It is the hardest of all minerals.

Back Next

Page 32: Earth science day one

Second scale

• Which rock scratches the surface of which rock?

• Feldspar will scratch Gypsum

Page 33: Earth science day one

Nice web site

• http://itc.gsw.edu/faculty/tweiland/sedrx2.htm

Page 34: Earth science day one

Dr Skaggs suggest’s . . .

13 softer than 21

based on 21

scratches 13

13 does not

scratches 21

finger nail

at Calcite

Page 35: Earth science day one

Use this principle

any thing I can scrathe wih my finger nail

3 below fingernailso now build up to finger nail

any thing I can scrathe wih my penny

3 below Penny (copper)so now build up to copper

any thing I can scrathe wih my glass

3 below glassso now build up to glass

Page 36: Earth science day one

• Do you know the difference between a rock and a mineral? Minerals are the building blocks of rocks. Here are some of the basic characteristics of minerals to help you understand what they are:

Page 37: Earth science day one

They are . . .

• Naturally occurring• Homogeneous• Inorganic• Solid • Ordered internal arrangemnt of atoms• (crystals or glasses)• Distinctive chemical composition

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caesium chloride unit cellthis structure is more likely to be formed from two elements whose ions are of roughly the same size (for example, ionic

radius of Cs+ = 167 pm, and Cl− = 181 pm).

Page 39: Earth science day one

.

• Minerals are inorganic; they are not alive and they are not plants or animals. An example of a rock that is not a mineral is coal. Coal is a substance formed from decayed plants and animals. Therefore, coal is not considered a mineral.

Page 40: Earth science day one

• Minerals are found in the earth or are naturally occurring substances. They are found in dirt, rocks, and water. They are not made by man

• A zincblende unit cell

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• Minerals are chemical substances. Some minerals like gold or silver are made of only one element. Other minerals, like quartz and calcite, are combinations of two or more elements.

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• Minerals always have the same chemical makeup. For example, quartz will always consist of one part silicon (an element) two parts oxygen (another element).

Page 43: Earth science day one

• Minerals always have the same chemical makeup. For example, quartz will always consist of one part silicon (an element) two parts oxygen (another element).

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• About 2,000 minerals have been found. Oxygen is part of many minerals. Minerals containing oxygen make up almost half of the earth's crust. Quartz is a common mineral. Other common minerals are feldspar, mica, and horneblend. Many rocks are made of these common minerals

Page 45: Earth science day one

• Some minerals are rare and expensive. They are called gems . Diamonds, rubies, and emeralds are good examples of such minerals. Gold and silver are also minerals. Together, these natural substances are used to make beautiful jewelry

Page 46: Earth science day one

A rock

• Is a naturally occurring, inorganic solid consisting of an aggregate of mineral grains , pieces of older rocks, or a mass of natural glass

Page 47: Earth science day one

Please complete page 8

Minerals Rocks Other

. .

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Lastly page 12-exercise 5

• Please identify all 24 sample according to cleavage

Page 49: Earth science day one

Click here to go back to the main pageCleavage is the tendency of a mineral to break along smooth planes parallel to zones of weak bonding.

Page 50: Earth science day one

• Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of weakness and break irregularly. See the picture below:

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“without a definite shape”

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Mineral Type of Breakage

Halite

CLEAVAGE

Cleavage in three directions at right angles (90o). Cubic cleavage.

Page 53: Earth science day one

CalciteCLEAVAGE

Cleavage in three directions not at right angles (120o and 60o).

Rhombohedral cleavage.

Page 54: Earth science day one

Calcite = CaCO3

• Rhombic or elongated crystals

• Reacts with HCl- • Specific gravity = 2.71• Cleavage=3 directions not at 90o

Page 55: Earth science day one

Gypsum

gypsumCLEAVAGE

Cleavage in one direction.

Page 56: Earth science day one

Calcium sulfate-dihydrate

• Gypsum=CaSO4.2H20

• Occurs in crystals or gray or white, earthly masses –alabaster

Colorles, white and gray• Hardness = 2• Perfect cleavage in one direction-may show

two other directions not at 90 degrees

Page 57: Earth science day one

Muscovite

CLEAVAGECleavage in

one direction.

Page 58: Earth science day one

KAl2 (AlS3010)

• Can be pealed into transparent, elastic sheets• Specific gravity = 2.66• Streak = yellow• Perfect cleavage in one direction• Hardness= 2-2.55

Page 59: Earth science day one

FeldsparCLEAVAGE

Cleavage in two directions at right

angles.

Page 60: Earth science day one

Quartz

FRACTURE

Mineral does not exhibit cleavage, it breaks or fracture

in an irregular manner.

Page 61: Earth science day one

quartz

• Conchoidal fracture• Hardness = 7• Elongated six sided crystals• Specific gravity = 2.65