Presentation is loading. Please wait.

Presentation is loading. Please wait.

ROCKS.

Similar presentations


Presentation on theme: "ROCKS."— Presentation transcript:

1 ROCKS

2 Are classified according to the environment in which they _________
form

3 Types of Rocks: ________ ________ ________
igneous Types of Rocks: ________ ________ ________ sedimentary metamorphic

4 IGNEOUS ROCKS

5 Where Does Igneous Rock Form?

6 I. FORMATION OF IGNEOUS ROCKS

7 solidification crystallization
A. Igneous rocks form directly from the _____________ and _____________ crystallization

8 of _____molten rock to form _______ rock
liquid of _____molten rock to form _______ rock solid

9 FOUNTAINING

10 FISSURE ERUPTION

11

12 LAVA FLOW

13

14 LAVA FLOW OVER A ROAD

15 LAVA FLOW THROUGH FORREST

16 Kilauea, HI 2003

17 Kilauea, HI , 2003

18

19 Mt. ST. Helens

20 Volcanic crater

21 crazy vulcanist

22 SKY LIGHT

23

24

25

26

27

28

29 B. _____________ is the process when a liquid rock cools,
crystallization B. _____________ is the process when a liquid rock cools,

30 and it changes to a solid made of ___________________
INTERGROWN CRYSTALS

31

32 GRANITE MICROSCOPIC VIEW

33 2. CLASSIFICATION OF IGNEOUS ROCKS:

34 A. 2 characteristics that are used to classify igneous rocks:

35 texture 1. ______________ 2. ______________ mineral composition

36

37 B. Texture of an igneous rock describes the

38 size shape arrangement
_________, __________ and ____________ of the mineral crystals it was made from. arrangement

39 C. The ______ of the crystals depends on the _______________________
size C. The ______ of the crystals depends on the _______________________ Rate of cooling

40 Slow cooling = ____________
large crystals

41

42 MINERAL CRYSTALS

43 GABBRO

44 Fast cooling = ____________
fine crystals Or no crystals (glassy)

45 GLASSY TEXTURE: OBSIDIAN

46 BASALT: FINE CRYSTALS

47 BASALT MICROSCOPIC VIEW

48 Granite: Coarse crystals Basalt: Fine crystals (Microscopic views)

49 FINE CRYSTAL: RYOLITE

50 3. EXTRUSIVE IGNEOUS ROCKS:
Extrusions A. _____________ occurs when molten (liquid) rock flows out of the earth as ________________ lava

51 lava magma

52 And cools __________ quickly

53 to form fine or no ____________ crystals

54 Vesicular basalt gas pockets

55 frothy texture (vesicular) This rock if full of gas pockets

56 B. To form magma, ____________ must be melted. minerals

57 pressures temperatures C. Minerals melt at different
____________ and ___________ temperatures pressures

58 D. Igneous rocks of different
____________ composition

59 Can form from the same body of ____________
magma

60 4. INTRUSIVE IGNEOUS ROCKS:
Intrusions A. _____________ occurs when molten rock beneath the surface (magma)

61 cools ____________ to form _____________ slowly coarse crystals

62 Granite: Coarse crystals Basalt: Fine crystals (Microscopic views)

63

64 low light (granitic) 5. FELSIC
A. Igneous rocks of the continental crust are rich in _________ density _________ colored minerals low light (granitic)

65 high dark (basaltic) 6. MAFIC
A. Igneous rocks of the ocean floor are rich in _________ density _________ colored minerals high dark (basaltic)

66

67 Comparing Oceanic Crust To Continental Crust

68 low density light color granitic felsic thick Continental Crust: 1. 2.
3. 4. 5. low density light color granitic felsic thick

69 high density dark color basaltic mafic thin Oceanic Crust: 1. 2. 3. 4.
5. high density dark color basaltic mafic thin

70 Complete the Activity Use this diagram in your ESRT to answer the following: What is the temperature for the interface between the following… inner core and outer core? 6250° C Outer core and stiffer mantle? 5000° C Stiffer Mantle and athenosphere? 2600° C Asthenosphere and lithosphere? 750° C

71 What is the depth of the interface between the stiffer mantle and the outer core? 2900 KM State the relationship between depth and pressure :As depth increase pressure increases State the relationship between depth and temperature: As depth increases temperature increases

72

73 When rocks melt, bonds broken. Crystalline solid no longer exists.
MELTING ROCKS AND CRYSTALLIZING MAGMA Rock magma magma rock When rocks melt, bonds broken. Crystalline solid no longer exists.

74 Hot liquid contains still solid fragments
MELTING ROCKS AND CRYSTALLIZING MAGMA Rock magma magma rock Hot liquid contains still solid fragments Minerals melt at different temperatures Melting causes changes in magma composition

75 Cooling of hot liquid allows crystallization of minerals
MELTING ROCKS AND CRYSTALLIZING MAGMA Rock magma magma rock Cooling of hot liquid allows crystallization of minerals Bonds are re-established Crystalline structure grows until edges touch adjacent crystals Minerals crystallize at different temperatures

76 OK……….. TAKE OUT YOUR REFERENCE TABLE

77


Download ppt "ROCKS."

Similar presentations


Ads by Google