bab.iib. batbeku-rock forming minerals

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FELDSPARS (two varieties to identify) All have two directions of cleavage. 1. PLAGIOCLASE (2 types to identify) (Ca,Na)(Si,A Have striations on cleavage planes (end at edge of cleavage plane). a. OLIGOCLASE (white) Na-rich feldspar b. LABRADORITE (gray to black) Ca-rich feldsp LABRADORITE OLIGOCLASE STRIATIONS

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Page 1: Bab.iib. Batbeku-rock Forming Minerals

A. FELDSPARS (two varieties to identify)All have two directions of cleavage.1. PLAGIOCLASE (2 types to identify) (Ca,Na)(Si,Al)4O8

Have striations on cleavage planes (end at edge of cleavage plane).a. OLIGOCLASE (white) Na-rich feldsparb. LABRADORITE (gray to black) Ca-rich feldspar

LABRADORITEOLIGOCLASE

STRIATIONS

Page 2: Bab.iib. Batbeku-rock Forming Minerals

Labradorite has labradorescence or chatoyance.

LABRADORITE

Page 3: Bab.iib. Batbeku-rock Forming Minerals

A. FELDSPARS (two varieties to identify)All have two directions of cleavage.2. ORTHOCLASE (pink, tan or white) KAlSi308

Has stringers that go through the mineral - looks superficially like striations.

Look at display so that you know what striations are.

ORTHOCLASE

Page 4: Bab.iib. Batbeku-rock Forming Minerals

B. FERROMAGNESIANS (iron and magnesium silicates)All have two directions of cleavage.1. AMPHIBOLES (2 types to identify) Cleavage planes intersect forming 124o and 56o

cleavage angles. Crystals usually long and thin.

a. HORNBLENDE (black)

Cleavage Angles

Page 5: Bab.iib. Batbeku-rock Forming Minerals

b. ACTINOLITE (greenish gray or grayish green)Crystals usually in radiating masses (check with me if not visible!)

ACTINOLITE

Page 6: Bab.iib. Batbeku-rock Forming Minerals

2. PYROXENES (1 to identify) Cleavage planes intersect forming

88o and 92o cleavage angles. Crystals usually short and stubby.

a. AUGITE (greenish black)

AUGITE

Page 7: Bab.iib. Batbeku-rock Forming Minerals

C. MICAS (3 to identify)All have one direction of cleavage, producing

platy appearance.1. MUSCOVITE (white-silver)2. BIOTITE (brown)3. CHLORITE (green) - may not look like the

other micas in terms of plateyness.

Page 8: Bab.iib. Batbeku-rock Forming Minerals
Page 9: Bab.iib. Batbeku-rock Forming Minerals
Page 10: Bab.iib. Batbeku-rock Forming Minerals

CHLORITE

Page 11: Bab.iib. Batbeku-rock Forming Minerals

D. QUARTZ (SiO2)Hardness is 7.Can be many colors due to impurities. Displays conchoidal fracture.

ROSE QUARTZ AMETHYST

Page 12: Bab.iib. Batbeku-rock Forming Minerals

CONCHOIDAL FRACTURE

Page 13: Bab.iib. Batbeku-rock Forming Minerals

E. OLIVINEOlivine is olive green.Granular appearance.May be able to see conchoidal fracture of grains

with hand lens.

Page 14: Bab.iib. Batbeku-rock Forming Minerals

F. CALCITE (CaCO3)Fizzes or effervesces in HCl.Three directions of cleavage not at right angles

(rhombohedral cleavage).Clear pieces may exhibit double refraction.

RHOMBOHEDRALCLEAVAGE HCl ACID REACTION

Page 15: Bab.iib. Batbeku-rock Forming Minerals

DOUBLE REFRACTION

Page 16: Bab.iib. Batbeku-rock Forming Minerals

G. GARNETReddish-brown color (but can be others).Has hackly fracture, no cleavage.Roundish crystals with 12-24 flat faces

readily visible in most cases.

Page 17: Bab.iib. Batbeku-rock Forming Minerals

H. STAUROLITECrystals usually twinned ("fairy crosses").