Looking at the natural hazards, climate changes, mineral resources, impact of environmental developments, changes in the earth's geography, etc. Base level study of earth. Internal and external process
Aristotle
Concluded that the position of land and sea had changed over a long period of time as fossils from rocks were similar to those found on the beach, indicating the fossils were once living animals
Copernicus
The earth revolves around the sun
JamesUssher (Catastrophism)
Catastrophe believer. Landscapes are formed due to catastrophe
JamesHutton (Uniformitarianism)
Theory of the earth. "Physical, chemical, and biological laws that operated today have also operated in the geologic past"
Siccar Point
Tectonically disturbed
Horizontal - Vertical
Vertical beds overlaid by horizontal beds
Earth Science
Different process of geology
Geosciences
Earth science that is partnered with other disciplines of science
NebularHypothesis
The solar system evolved from an enormous rotating cloud called the solar nebula
The nebula was composed mostly of hydrogen and helium
5 billion years ago, the nebula began to contract
It assumed a flat, disk shape with the protosun (pre-Sun) at the center
Inner planets begin to form metallic and rocky clumps
Larger outer planets began forming from fragments with a high percentage of ice
Spheres of Earth
Hydrosphere
Atmosphere
Biosphere
Geosphere
Hydrosphere
Ocean is the most prominent feature, covering 71% of Earth's surface and holding about 97% of Earth's water
Also includes fresh water found in streams, lakes, and glaciers, as well as that found groundwater
Atmosphere
Thin, tenuous blanket of air, with one half lying below 5.6 kilometers (3.5 miles)
Biosphere
Includes all life, concentrated near the surface in a zone that extends from the ocean floor upward for several kilometers into the atmosphere
Geosphere
Rocks and minerals on Earth
Plate tectonics
The theory that proposes the Earth's outer shell consists of individual plates that interact in various ways and thereby produce earthquakes, volcanoes, mountains, and Earth's crust itself
MapsLatitude and Longitude are lines on the globe that are used to determine location
Latitude is the distance north or south of the equator, measured in degrees
Longitude is distance east or west of the prime meridians, measured in degrees
Topographic maps represent Earth's surface in three dimensions, showing elevation, distance directions, and slope angles
Contourlines are lines on a topographic map that indicate an elevation
Contourinterval is the distance between adjacent contour lines
A system is a group of interacting parts that form a complex whole
Closed systems are self contained
Open systems allow both energy and matter to flow in and out of the system
Sources of Energy
Sun drives eternal processes such as weather, ocean circulation and erosion processes
Earth's interior drives Internal processes including volcanoes, earthquakes, and mountain building
Matter
Anything that occupies space and has mass
Elements
The basic building blocks of minerals, with over 100 known
Atoms
The smallest particles of matter, containing protons, neutrons, and electrons
Nucleus
The central part of an atom, containing protons and neutrons
States of Matter
Solid
Liquid
Gas
Energy Levels/Shells
Surround the nucleus and contain electrons
Atomic Number
The number of protons in the nucleus of an atom
Isotopes
Have the same number of protons but varying numbers of neutrons, with different mass numbers
Mass Number
The number of neutrons and protons in the nucleus of an atom
Atomic Bond
Forms when an atom's outermost energy level does not contain a maximum number of electrons
Types of Atomic Bonds
Ionic
Covalent
Metallic
Compound
Two or more elements that are chemically combined in specific proportions
Ion
An atom that gains and loses electrons
Mineral Properties
Color - small amounts of different elements can give the same minerals different colors.
Streak - the color of a mineral in its powdered form
Luster - used to describe how light is reflected from the surface of a mineral.
Crystalform - the visible expression of a mineral's internal arrangement of atoms
Crystal Growth
Crystallization occurs by the addition of atoms to a crystal face, as the outer layer of atoms on a crystal are never completed and can accept additional atoms
Luster
The visible expression of a mineral's internal arrangement of atoms
Hardness
A measure of the resistance of a mineral to being scratched
Mohs Scale
Consists of 10 minerals arranged from 10 (hardest) to 1 (softest)
Cleavage
The tendency of a mineral to cleave, or break, along flat, even surfaces
Fracture
The uneven breakage of a mineral
Density
A property of all matter that is the ratio of an object's mass to its volume
Destruction of crystal
Heat and pressure cause some crystals structures to collapse and new minerals with a more dense, compact atomic structure to form in their place