Have solid surfaces, dense and metallic core, nitrogen and carbon dioxide are abundant in their atmosphere
Terrestrial Planets
Mercury, Venus, Earth, and Mars
Jovian Planets
Have gaseous surfaces, less dense core supposedly molten rock, hydrogen and helium are vastly present in its atmosphere
Jovian Planets
Jupiter, Saturn, Uranus, and Neptune
Six factors that make Earth habitable
Closeness to the Sun
Earth's Atmosphere
Earth's consistent temperature
Earth's moon
Diversity of Life
Water
Closeness to the Sun
Earth's distance from the sun is 151.2 million kilometers, which enables Earth to get much-needed heat
Earth's Atmosphere
Five layers of atmosphere (smallest-largest), Ozone Layer helps to warm the planet by day and cools it at night
Without the Moon, 1 day would be 4 hours instead of 24 hours
Diversity of Life
Food chain sustains the survival and evolution of organisms, Biodiversity and Evolution are products of the interaction of organisms with their environment
Earth is covered 71% by water
Atmosphere
Gaseous layer above Earth's surface, primarily composed of 78% nitrogen and 20.9% oxygen, supports life of humans, plants, and animals, protects us from harmful ultraviolet solar radiation
Hydrosphere
The water part of the Earth which circulates among oceans, continents, glaciers, and atmosphere, Cryosphere is the frozen water part of the Earth system
Geosphere
The solid Earth, consisting of the entire planet from the center of the core to the outer crust, includes the rocks and minerals - from the molten rock and heavy metals in the deep interior of the planet to the sand on beaches and peaks of mountains
Biosphere
All forms of life exist; in the sea, on land, and in water, they are all connected
Geology is the study of the Earth: its history, nature, materials and processes
Geologist
Scientists who study the Earth: its history, nature, materials and processes
Mineralogy
The study of the chemistry, crystal structure and physical properties of the mineral constituents of rocks
Mineralogist
A person who studies minerals
Petrology
The scientific study of rocks
Petrologist
Person who study rocks
Mineral
A naturally occurring, inorganic, homogeneous solid, with a definite chemical composition, and an ordered crystalline structure
Characteristics of Minerals
Natural Occurring
Chemically Inorganic
Homogenous Solids
Crystalline Structure
Definite Chemical Composition
Physical Properties of Minerals
Color
Streak
Hardness
Cleavage
Crystalline
Diaphaneity
Luster
Tenacity
Specific Gravity
Rock
A naturally occurring solid aggregate of one or more minerals
Igneous Rocks
Formed from the crystallization and solidification, Latin word "Ignis" which means "Fire"
Sedimentary Rocks
Formed from the accumulation of sediments, word "Sediments" means "to settle at the bottom"
Types of Sedimentary Rocks
Clastic - Formed from accumulation of clasts (little pieces of broken rocks and shells)
Chemical - Formed when dissolved minerals precipitate from a solution
Organic - Made from the remains of plants and animals and may contain fossils
Formation of Sedimentary Rocks
1. Erosion
2. Deposition
3. Cementation
Metamorphic Rocks
Rocks that are formed from igneous or sedimentary, Meta means "change" and morph means "form"
Types of Metamorphism
Contact - Mainly heat due to contact with magma
Regional Metamorphism - Due to the changes in pressure and temperature over large region in the crust
Types of Metamorphic Rocks
Foliated - Appeared banded or layered
Non-foliated - The grains are random and do not split into layers
Exogenic Processes
Geologic processes that occur on the surface of the earth
Exogenic Processes
Weathering
Erosion
Mass Wasting
Sedimentation
Weathering
Disintegration of rocks, soils, and minerals together with other materials through contact in Earth's subsystem
Types of Physical Weathering
Release of Pressure
Frost Wedging
Abrasion
Biological Activity
Human Activity
Types of Chemical Weathering
Dissolution
Hydrolysis
Oxidation
Erosion
The process which Earth's surface is worn away by wind, water, or ice, Erosion moves rock debris or soil from one place to another