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Geology 1303Block 2 Minerals Rock Cycle Igneous Rocksincluding volcanoes

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Elements combine with each other to form a wide variety of minerals (chemical compounds) ... it possible for two different minerals to have the same chemical ... – PowerPoint PPT presentation

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Title: Geology 1303Block 2 Minerals Rock Cycle Igneous Rocksincluding volcanoes


1
Geology 1303-Block 2MineralsRock
CycleIgneous Rocks-(including volcanoesplutons)
Sedimentary RocksMetamorphic rocksExam 2 Oct
18th WED -To be Confirmed
2
  • What is a mineral?
  • How do we differentiate a mineral from a piece of
    wood or a human?
  • What is a rock?

3
Minerals
  • What is a mineral?
  • Naturally occurring (not man-made)
  • Inorganic
  • Solid (not made of liquid or gas) with a definite
    chemical structure which give it unique physical
    properties.

4
Minerals vs. Rocks
  • There are nearly 4000 known minerals - but most
    rocks are formed by only a few dozen minerals.
  • Rocks are aggregates (mixtures) of minerals. So .
    . . minerals are the building blocks of rocks.
  • A question for the future How do minerals come
    together to form a rock?

5
Composition and Structure of Minerals
  • To understand how minerals form, we need to
    understand the characteristics of elements and
    atoms.
  • Chemical Elements
  • Elements are the basic building blocks of
    minerals. There are over 100 known elements.

6
Composition and Structure of Minerals
  • Atoms
  • smallest particle of matter that exhibits all the
    characteristics of an element.
  • Atoms are made up of
  • Nucleus, which contains Protons (atomic number)-
    positive electrical charges and Neutrons -
    neutral electrical charges (P N atomic mass)
  • Shells which surround the nucleus and contain
    Electrons - negative electrical charges
  • The weight (density) of an element depends on the
    number of protons and neutrons in the nucleus.

7
Combining Elements to Form Minerals
  • Elements combine with each other to form a wide
    variety of minerals (chemical compounds)
  • Atoms combine chemically by gaining, losing, or
    sharing and electron with other atoms. (opposites
    attract) (pg-26)
  • The new mineral (compound) will have very
    different physical properties from the elements
    that combined to form it.

8
Combining Elements to Form Minerals
  • Since rocks are mixtures (not chemical
    combinations) of minerals, minerals keep their
    physical properties within a rock.
  • Is it possible for two different minerals to have
    the same chemical composition?
  • YES! Both diamond and graphite are made of
    carbon. The difference between these two
    minerals is the way in which the carbon atoms are
    arranged.

9
Mineral Properties
  • Minerals have lots of different properties that
    help us identify them.
  • Crystal form, Luster, Color,
  • Streak, Hardness, Cleavage,
  • Fracture, Specific gravity,
  • Taste, Smell, etc.

10
Rock Forming Minerals
  • The most common rock forming minerals are
    composed of 8 elements
  • Oxygen (O) , Silicon (Si),
  • Aluminum (Al) , Calcium (Ca) , Sodium (Na) ,
    Potassium (K)
  • Iron (Fe) and Magnesium (Mg)
  • There are just a few dozen minerals that we call
    the rock-forming minerals.

11
Composition of the Crust
  • The most abundant elements in Earth's crust are
  • Oxygen (46.6 by weight)
  • Silicon (27.7 by weight)

The crust
12
Silicate Minerals
  • Silicate minerals, minerals built primarily from
    silicon-oxygen tetrahedrons, are the most common
    rock-forming minerals.
  • Silicate minerals are grouped according to how
    the tetrahedrons are arranged in the mineral.

13
Silicate Mineral Groups
  • Olivine - independent tetrahedrons (Mg, Fe)
  • Pyroxene group - tetrahedrons are arranged in
    chains (Mg, Fe)
  • Amphibole group - tetrahedrons are arranged in
    double chains (Mg, Fe, Ca)
  • Micas - Tetrahedrons are arranged in sheets
  • Two common types of mica
  • Biotite (dark) (K, Mg, Fe, Al),
  • Muscovite (light) (K, Al)

14
Silicate Mineral Groups
  • Feldspars - Three-dimensional network of
    tetrahedron
  • Two common types of feldspars
  • Orthoclase (K, Al)
  • Plagioclase (Ca, Na)
  • Most plentiful mineral group
  • Quartz - three-dimensional network of
    tetrahedrons (SiO2)

15
Mineral Color
  • Mineral color is often governed by presence of
    Mg, Fe (dark) or absence of these elements
    (light).

16
Non-Silicate Minerals
  • Major groups
  • Oxides (FeO2), Sulfides (PbS), Sulfates (CaSO4),
  • Halides,
  • "Native" elements (gold),
  • Carbonates (limestone, marble) (CaCO3)

17
Mineral Resources
  • Ore - rock that contains useful metallic minerals
    that can he mined at a profit.
  • Since 98 of the Earth's crust is made up of 8
    elements, an element/mineral has to be
    concentrated at levels above normal for
    profitable mining.

Rocks
18
A Rock is anAggregateof Minerals
Quartz
Amphibole
Feldspar
19
Structureof an Atom
Electron
Nucleus
Nucleus (neutrons protons)
20
Chemical Compound
Na
Cl-
NaCl
21
Silicon-OxygenTetrahedron(SiO4)
Isolated Tetrahedrons (Olivine)
22
Tetrahedron Arrangement
Single-Chain
Double-Chain
Sheet
Pyroxene
Amphibole
Mica
23
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29
Mohs hardness scale
  • 10. Diamond 4. Fluorite
  • 9. Corundum 3. Calcite
  • 8. Topaz 2. Gypsum
  • 7. Quartz 1. Talc
  • 6. Potassium Feldspar
  • 5. Apatite

30
  • Please do not use WebCT for email
  • aellis_at_utep.edu
  • Minerals Cont.
  • Rocks and the Rock Cycle

31
For Next Time
  • How do minerals "mix" together to form rocks?
  • What is the rock cycle ?
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