a volcanic eruption is the expulsion of gases, rock fragments, and molten lava within the earth through a vent onto the Earth's surface or into the atmosphere.
Magma is extremely hot liquid and semi-liquid rock located under Earth's surface.
the magma blasts into the air and breaks apart into pieces called tephra.
Tephra can range in size from tiny particles of ash to house-size boulders.
Types of volcanoes
composite volcanoes
stratovolcanoes
cinder or scoria cones
shield volcanoes
caldera volcanoes
submarine volcanoes
submarinevolcanoes also known as seamounts (underwater mountains).
magmaticchamber is a deposit of molten rock or magma that lies beneath the earth's crust at high pressure.
volcanicchimney is the space that communicates the magmatic chamber with the exterior.
crater it is the hole or opening of the volcano.
volcaniccone the various liquid, solid, and gaseous materials expelled from the volcano from the earth's interior.
secondarycones in the event that fissures are created by the pressure exerted by the gases during the eruption.
parts of a volcano
magmatic chamber
volcanic chimney
crater
volcanic cone
secondary cones
the formation of a volcano can take thousandsofyears. it is a very slow proccess.
the fact that a volcano is inactive does not guarantee that it will not be able to start a volcanic eruption process.
the temperature of the lava expelled by the volcano can reach up into 1000 degrees celsius.
volcanoes are also in space.
volcanoes can be formed by the constant movement of tectonic plates on the earth.
the lithosphere weakens and allows magma to appear in the earth's interior.
a volcano is a crack, openingorhole that occurs in the earth's crust, which allows lava or magma to escape.
a caldera is a large, usually circular volcanic depression.
a shield volcano is a type of volcano named for its low profile.
a stratovolcano or composite volcano is a conical volcano that is built up from layers of lava and ash
cinder cones are the most commons types of volcanoes.
cinder cones are also known as ashcones.
global warming is the long term warming o the planet's overall temperature.
The greenhouse effect is when the sun’s rays penetrate the atmosphere, but when that heat is reflected off the surface cannot escape back into space.
The Greenhouse Gases
Watervapor
chlorofluorocarbons
nitrousoxide
methane
Carbondioxide
Climatechange refers to changes in weather patterns and growing seasons around the world.
The cause of current climate change is largely humanactivity, likeburning fossil fuels, likenaturalgas, oil, andcoal.
effects of climate change
drought
meltingofseaice
sealevelsrise
hurricane
Ways we can help prevent Climate Change
Reducewaterwaste
Driveafuel-efficientvehicle.
Don’twastefood
Planttrees
Reduceplastic
Spreadtheword
Temperature Factors (LADBWOC!)
Latitude
Altitude
Distance to a Body of Water
Ocean Currents
Precipitation Factors
Topography
Prevailing Winds
Latitude is the most significant factor for determining climate
As you go up in altitude, you go down in temperature and sometimes precipitation
GEOTHERMAL ENERGY IS HEAT WITHIN THE EARTH THE WORD GEOTHERMAL COMES FROM THE GREEK WORD “GEO” (EARTH) ANDTHERME (HEAT).
2 types of geothermal energy
geothermalpowerplants
geothermalheatpumps
GeothermalReservoirs are Naturally occurring large areas of hydrothermal resources.
GeothermalHeatPumps Tap into heat close to the earth's surface to heat water or provide heat for buildings.