earth science chap 1 Flashcards
Steps of the scientific method
Observation
Hypothesis
Test
Scientific method deffination
The orderly process by which explanations for observations made in nature are accepted or rejected
Observation
Asking questions and or collecting information
Hypothesis
A testable explanation for a set of observations or information
Tests
Models or experiments that determine the feasibility of a hypothesis
The earth system
Solid earth Hydrosphere Atmosphere Biosphere All works together to influence each other
Is earth a closed system?
Contained no outside influences
No it is an open system
Gets energy from the sun
What is a mineral?
Naturally occurring
Inorganic solid
Definite chemical composition
Parts of the earth
Crust Mantle Core Inner core Outter core
Elements
Simplest chemical; cannot be broken down
Atoms
Smallest piece of an element that has a specific structure.
Protons
Positive
Electrons
Negative
Neutrons
Zero charge
Ions
Atoms with extra or too few electrons has net charge.
Ionic bonds
Opposite charges
Compound
Chemical combination of two or more elements held together by bonds
Covalent
Share bonds
Metallic
Covalent on steroids; share a lot of bonds
Crystals
Atoms arranged in regular, ordered , and repeated patterns
Crust
we stand on
Mantle
most of planet, more dense, ooy gooy , squishy
Core
inter part , most dense
Inner core
very hot
Outter core
internal heat engine
Mafic Silicates
Darker; oceanic crust
Felsic silicates
lighter; contentail crust
Pluntonic rock; phaneritic texture; instrusive
slowly cooling rocks, you can see the crystals
Volcanic rock; Aphanitic texture; extrusive
rapid cooling rocks, you can’t see crystals
Steps in sedimentary rocks
- Weathering
- Transport
- Deposition
- Linlfication
Weathering
breaking older rocks down into particle and solutions- response of earth material to changes in the environment
Transport
Made in high spot moved to low spot
Deposition
sediments are deposited within broad regional low spots called basins, and sedimenntary rocks form there over time
Lithlfication
converting loose sediment into solid rock. Burial lead to - compaction, cementation
SEdimentary rock
broken down igneous
Igneous Rock
heat creates them; starts as megma then crysratlizes
metamorphic rock
starts as sedimentary; exposed to heat and becomes metamorphic. if it gets to hot it turns back into sedimentary or igneous
What rocks have big crystals?
Igneous
what rocks look grainy and sandish and have rocks in them?
sedimentary
what rocks have texture and are layered?
Metamorphic
important characteristics of a sedimentary rock
Texture and componets
Metamorphic Rocks
Form because of heat and pressure change when it is solid
convection
divergent boundaries
two types of metamorphic rock
regional and contact
Mechanical weathering
Big to little rocks
Low grade metamorphic rock
Slate
Chemical weathering
Cheimcal reaction; water
Medium grade metamorphic rock
schist
high grade metamorphic rock
gneiss
perpenduilar stress fracture
was being pressed downward.