Earth Science Rocks Flashcards
Properties of Rocks
- Naturally occurring
- Solid
- May contain organic materials
- NO definite chemical composition
Example of “may contain organic materials”
Fossils, shells, teeth, bones
Rocks may compose _________________.
Two or more minerals
Example of a rock containing two or more minerals
Granite (igneous rock) - feldspar, mica, quartz
Any naturally occurring solid mass or aggregate of minerals or mineraloid matter.
Rocks
Three types of rocks
Igneous Rocks
Sedimentary Rocks
Metamorphic Rocks
Rocks that came from melted rock material (magma) or lava.
Igneous Rock
Type of Rock. When the magma cools down, it solidifies (namumuo) forming yung minerals sa loob. (Crystallization)
Igneous Rock
Two Classification of Igneous Rocks
Intrusive, Extrusive
Classification of Igneous Rock. Crystallize below Earth’s surface, and the slow cooling that occurs there allows large crystals to form.
Intrusive Igneous Rocks
Classification of Igneous Rock. Erupt onto the surface where they cool down quickly to form small crystals.
Extrusive Igneous Rocks
Intrusive igneous rocks are also known as ________
PLUTONIC
Extrusive igneous rocks are also known as ________
VOLCANIC
Examples of Intrusive Igneous Rocks
Granite, Diorite, Pegmatite, Gabbro
Examples of Extrusive Igneous Rocks
Obsidian, Basalt, Andesite, Pumice, Rhyolite
Cooling time of intrusive and extrusive:
Intrusive: Thousands of years
Extrusive: Seconds to months
What does categorized “By Texture” mean?
Depends on the size of the crystals
By Texture. One that has large crystals.
Course-Grained (Part of Intrusive Rocks)
Examples of Course-Grained Rocks
Granite, Diorite, Gabbro, Peridotite
By Texture. One that has small crystals.
Fine-Grained (Part of Extrusive Rocks)
Examples of Fine-Grained Rocks
Rhyolite, Andesite, Basalt, Komatiite
By Chemical Composition. Grey to Black, Black to Olive Green Silicates.
Mafic (Basaltic), Ultramafic
By Texture. Mix, it has large embedded in small crystals.
Porphyritic
By Texture. No crystals, kapag sobrang bilis ng cooling this may happen.
Glassy
Examples of Glassy Rocks
Pumice, Obsidian
Not used often. By Texture. Butas-butas
Vesicular
Examples of Vesicular
Pumice, Scoria
By Chemical Composition. Light, Light to Dark Grey Silicates.
Felsic (Granitic), Intermediate (Andesitic)
By Chemical Composition. Grey to Black, and Black to Olive Green
Mafic (Basaltic), Ultramafic
Rocks that are formed on or near the Earth’s surface. It is the accumulation of mineral or organic particles, and founded from solidification of sediments.
Sedimentary Rocks
Two MAIN Classifications of Sedimentary Rocks
Clastic (Detritus) SR, Organic (Dissolved) SR
The Chemical SR is UNDER the Organic SR
This classification is formed from mechanical weathering. Give examples.
Clastic SR: Conglomerate, Shale, Sandstone
This classification is formed from the accumulation of plants or animal debris. Give examples.
Organic SR. Chalk, Coal, Lignite, Limestone, Dolomite
Sedimentary Rocks texture depends on the _____________
Depends on the size of the particles
Classifications of Sedimentary Rocks.
Coarse, Medium Sized, Very Fine
In the sedimentary classification, give the types and examples.
Coarse: Conglomerate - Rounded Sediments
Breccia - Angular (May tusok-tusok)
Medium Sized: Sandstone
Fine: Siltstone
Very fine: Shale
Vry Vry Fine: Mudstone
An example of Sedimentary Rock that is made of organic materials:
Coquina
- It is the rocks formed in the ceiling 2. rocks formed from the ground 3. if both 1 and 2 connect it will be called _____
- Stalactites 2. Stalagmites 3. Column
These rocks were once igneous or sedimentary rocks. Nabubuo mula sa ibang bato through the process of ________.
Metamorphic Rocks, Metamorphism
Process of change in the structure, texture, or
composition of rocks to form the metamorphic rocks.
Metamorphism
What are the agents that causes metamorphism. Without these, the process would not work.
Heat and Pressure
The two types of metamorphism:
Contact Metamorphism & Regional Metamorphism
In this type of metamorphism, it will undergo the process if there is contact with heat (MAGMA). It also happens underneath the surface.
Contact Metamorphism
If there is too much heat close to the rocks, it would result to:
Melting
In this type of metamorphism, mas lamang ang PRESSURE, it usually happens at plate tectonic convergence zone. Unlike the other type, mas malaki ang bilang na nadadamay dito.
Regional Metamorphism
What does “Based on Texture” in classifying metamorphic rocks?
The arrangement of minerals.
Types of metamorphic rocks based on texture:
Non-Foliated Rocks & Foliated Rocks
These types of rocks (texture) are produced from contact metamorphism.
Non-Foliated Rocks
These types of rocks (texture) are produced from regional metamorphism
Foliated Rocks
These types of rocks (texture) are formed at LOW Pressure, HIGH Temperature. It has no cleavage.
Non-Foliated Rocks
Examples of Non-Foliated Rocks
Marble, Hornfels, Quartzite
This mean the parallel arrangement of certain mineral grains that gives the rock a striped appearance.
Foliation
These types of rocks (texture) are formed at HIGH Pressure. It contains cleavages.
Foliated Rocks
Examples of Foliated Rocks
Gneiss, Slate, (not sure Biotite)
The foliation in this rock is not seen with the naked eye.
Slate
This refers to the range of metamorphic change it undergoes, from low grade, or little metamorphic change; to high grade, or significant metamorphic change.
Metamorphic Grade
Low-grade metamorphic rocks tend to be ____________ and high-grade metamorphic rocks tend to be _____________.
Fine-Grained, Coarse-Grained
Metamorphic Grade; Increasing Pressure & Increasing Temperature:
Shale, Slate, Schist, Gneiss, Migmatite
Hornfels (Only almost requires heat)
Blueschist (only almost requires pressure)
_____ rock, also sometimes ________, is the
original rock from which younger rock or soil is formed.
Parent Rock; Substratum
Connect Parent Rocks to the Metamorphic Rocks
1. Shale
2. Quartz/Sandstone
3. Limestone/Dolomite
3. Granite/Gabbro
4. Coal
a. Marble
b. Slate
c. Gneiss
d. Quartzite
e. Anthracite
(b, d, a, c, e)
The Rock Cycle. What can be done to form Igneous Rocks?
Cooling/Crystallization of Magma (Lava)
The Rock Cycle. What can be done to Igneous Rock?
Melting —-> Magma
Heat & Pressure —-> Metamorphic Rock
Weathering & Erosion —-> Sediments
The Rock Cycle. What can be done to form Sediments?
W & E of Igneous, Sedimentary, & Metamorphic Rock
The Rock Cycle. What can be done to Sediments?
Compaction & Cementation (Lithification) —-> Sedimentary Rock
The Rock Cycle. What can be done to form Sedimentary Rocks?
Lithification of sediments
The Rock Cycle. What can be done to Sedimentary Rocks?
H & P —-> Metamorphic Rocks
W & E —-> Sediments
Melting —-> Magma
The Rock Cycle. What can be done to form Metamorphic Rocks?
H & P of Igneous & Sedimentary Rock
The Rock Cycle. What can be done to Metamorphic Rocks?
W & E —-> Sediments
Melting —-> Magma
The Rock Cycle. What can be done to form Magma?
Melting of Igneous, Sedimentary, & Metamorphic Rock
The Rock Cycle. What can be done to Magma?
Cooling/Crystallization —-> Igneous Rock