Rocks - North Rose-Wolcott Central School District

Rocks - North Rose-Wolcott Central School District

Rocks and Minerals

Minerals In order for a substance to be consider a mineral, it must have the following 5 characteristics:

Must be solid Must be inorganic Must be naturally occurring Must have a definite chemical composition Must have a definite crystal

shape Minerals are the basic building blocks of all rocks. Oxygen is the most abundant by mass and volume (46%, 94%)

Silicon is second in mass (28%) Mineral Properties All mineral properties are determined by the

INTERNAL ARRANGEMENT of ATOMS Please grab the three (3) pieces of paper on the side of the room.

Using a blue or black pen, please fill out the STEM survey. Properties Color easiest property to identify but the most

useless Many minerals have the exact same color but are completely different. Properties

Luster the way the mineral shines in reflected light Two types Metallic Looks like metal, gold or silver in color Nonmetallic Doesnt look

like metal Properties contd Streak color of the minerals powder when rubbed on a streak plate.

Will not always be the same color as the mineral sample Example Pyrite is gold in color but has a green/black streak Properties contd

Cleavage the tendency of a mineral to break, or cleave, in a flat plane - Properties contd Fracture Irregular breakage

Looks a lot like breaking apart a clod of dirt or a cookie. No pattern of breakage Properties contd Hardness resistance to being scratched

Follows Mohs Hardness Scale Types of Minerals Silicates made up of primarily silicon and oxygen Silica Tetrahedron basic building blocks

of all silicates (SiO4) Other types of Minerals Carbonates Iron Oxides -

Common Uses Feldspar used in ceramic and glass products, fertilizers, and soaps Gypsum used in drywall and plaster applications, cement, and fertilizer

Quartz used in electronics, jewelry, and in powder form can be used as a thickening agent Mica- used as electrical insulators, and as bonding agents in paints and flux in welding rods Fluorite used to make hydrofluoric acid, and

powdered as a fluorine agent in municipal water systems and toothpaste Sulfur used in manufacturing processes, such a drug production and vulcanization of rubber IGNEOUS ROCKS

Form by solidification and crystallization of melted minerals Plutonic formed underground -Also known as intrusive - Cools slowly- LARGE CRYSTALS - texture will be considered coarse

Volcanic forms aboveground - also known as extrusive - Quick cooling means fine to no crystals - Texture is considered fine or

glassy Obsidian Natural volcanic glass Forms when lava

cools very quickly Usually dark, but small pieces may be clear Fractures along curved (conchoidal)

surface Used as spear and arrow points, knives Types of Magma - Felsic

- light in color - low in density - contains a lot of feldspar - Rocks include granite, pegmatite, and pumice

-Mafic - dark in color - high in density - contains a lot of iron - Rocks include Gabbro, Basalt,

Vesicular gas pockets Rock Texture- texture is determined by crystal size not how the rock feels

-NO ONE CARES HOW YOU FEEL when it comes to texture Igneous Characteristics-MEMORIZE ME 1. Visible Scattered Crystals 2. Glassy texture

3. Visible gas pockets (vesicular) Sedimentary Rocks Sedimentary Rock- - formed from compaction and cementation of sediments or living organisms

THREE MAJOR TYPES Sedimentary Rocks - Clastic (fragmental) made of sediments of other rocks that have been broken down - Classified by the size of the sediments that

make up the rock Sedimentary Rocks Sedimentary Rocks Chemical(crystalline)- forms when water

dissolves minerals, evaporates and leaves the mineral behind Sedimentary Rocks Bioclastic (Organic) made from the parts of

living things, such as plants and animals Sedimentary Rocks Processes that create sedimentary rocks

- Compaction- pressing of sediments together by force Sedimentary Rocks Cementation- gluing sediments

together with some sort of natural process Super Cool Totally Groovy Cementation Animation

Sedimentary Rocks Stratification- when sediments pile up in layers Sedimentary Rocks

Fossils evidence of life, often found in sedimentary rocks Characteristics of Sedimentary Rocks

1. Visible Sediments Characteristics of Sedimentary Rocks 2. Dull, Earthy colors

Characteristics of Sedimentary Rocks 3. Visible fossils Characteristics of Sedimentary Rocks

4. Sediments in layers ESRT- Sedimentary Rocks Metamorphic Rocks

Formed by heat and pressure changing existing rocks Regional metamorphism that occurs over a large area that is exposed to heat and pressure - causes severe metamorphism

Regional Metamorphism- Metamorphic Rocks Regional Metamorphism- Metamorphic Rocks Contact- change that occurs when rocks

come in contact with heat only - Subtle changes - Deformation only Characteristics of Metamorphic Rocks

1. Bands of Crystals (color bands) Characteristics of Metamorphic Rocks 2. Deformation

Characteristics of Metamorphic Rocks 3. Foliation- crystals in flaky layers ESRT: Metamorphic Rocks

Rock Cycle Content resources

Diamond/Graphite Image: Sulfur - Pyrite-

Kaolin - Streak Image - Calcite - Cleavage - Fracture - Mohs Scale -

Mohs Image - Silica Tetrahedron -

Recently Viewed Presentations

  • Cascades-2


    Higher-frequency variations in B-angles are poorly correllated (by eye) between probes, and so are also poor timing markers!!! THA THE THD Notes: On-Board Spin Fit (3-s resolution) B- and E-field. DSL coordinates (Despun Spacecraft, z along L), ~ GSE. Spin...
  • The Early Use and Understanding of Heredity

    The Early Use and Understanding of Heredity

    Another early notion of heredity was blending inheritance, which proposed that offspring are a blend, or mixture, of parental traits. This idea suggested that the genetic material itself blends, much as blue and yellow pigments blend to make green paint.
  • Transition and the IEP - The Arc of Texas

    Transition and the IEP - The Arc of Texas

    Student postsecondary goals developed at the ages of 14 or 15 are generally more global than the ones developed at age 16, which will need to be more specific. All postsecondary goals should be measurable and should include all three...
  • Unit 1 Modern Inequalities - MR. BEST WORLD HISTORY

    Unit 1 Modern Inequalities - MR. BEST WORLD HISTORY

    8/26/89: DOROMAC passed. October 21: The Assembly declares a state of martial law to prevent future uprisings. November 2: The Assembly votes to make property of the Church available to the Nation. December 24: The Assembly decrees that Protestants are...
  • LWW PPT Slide Template Master

    LWW PPT Slide Template Master

    Project Management Essential skill of nursing informatics specialist Management of project from start to finish Skills Communication Team building Organizational planning Time and resource management Systems life cycle as backbone Systems Life Cycle Conception of system until implementation Analogous to...
  • Anglo Saxon Period 449 - 1066

    Anglo Saxon Period 449 - 1066

    Arial Lucida Sans Book Antiqua Wingdings 2 Wingdings Wingdings 3 Calibri Arial Black Bradley Hand ITC Apex Anglo Saxon Period 449 - 1066 BEOWULF: AN EPIC HERO Literary Characteristics of Anglo-Saxon period THE ELEGY Medieval Period 1066-1485 Canterbury Tales (cont)...
  • Introduction to GCSE History Starter: please fill in

    Introduction to GCSE History Starter: please fill in

    In the early Anglo-Saxon period, England was actually 7 separate Kingdoms. ... Made new laws, controlled circulation of pennies, granted land to his followers and could take land away (could raise people to title of thegn), had the power to...
  • 2.7 Redox Reactions - NZ Science Class Online

    2.7 Redox Reactions - NZ Science Class Online

    Iodate Iodine. H+ (aq) H. 2(g) Hydrogen ion Hydrogen gas ... as in the case of dichromate and the chromium ions. Oxidation Numbers. Oxidation numbers can be used to predict whether a species - the reactant and its product -...