LESSON 1-5 Flashcards
Makakapasa po ako sa ngalan mo Hesus. Amen.
A molten material beneath or within the Earth’s crust from which igneous rocks are formed.
What is magma?
A process in Earth’s crust where formation and movement of magma occur.
Magmatism
- Oxygen
- Silicon
- Aluminum
- Iron
- Calcium
- Sodium
- Magnesium
- Potassium
Magma is made up of 8 elements
Rocks begin to melt at a temperature between ___ and ____ degrees Celsius.
between 800 to 1200 degree Celsius
Origin of Magma
Earth has 3 solid part and 1 liquid part in order for magma to form some part of the Earth must get hot enough to melt rocks.
Magma forms when rocks reach temperatures high enough to melt them.
Processes that form magma by melting of mantle rock
- increase in temperature
- decrease in pressure
- addition of volatiles
Increase in temperature
minerals in the rock have different melting point
Decrease in pressure
Rocks beneath the earth remain solid when exposed to high pressure. During convection, rocks go upward, reducing the pressure.
Addition of volatiles (water, gases)
adding of impurities like water and gas lower the melting point of rocks.
Types of Magma Generation
Subduction zone
Hot spot volcanism
Magmatism along rift zones
Formed through dry partial melting of mantle
Basaltic
Formed through wet, partial melting of the mantle
Andesitic
Formed as a result of wet melting of continental crust
Rhyolitic
Factors that affects the viscosity of the magma
- Temperature
- Chemical composition/silica content
- Amount of dissolved gases
An eruption of molten rock, hot rock fragments and hot gases through a volcano, which is a vent in the Earth’s crust
Volcanic eruption
Takes place when magma’s temperature get very high under the Earth’s surface
How volcanoes erupt
Low gas content and low viscosity of magma (basaltic to andesitic magma) begin with fire fountains due to release of dissolve gases
Effusive/Non Explosive Eruptions
High gas content and high viscosity (andesitic to rhyolitic magma)
Explosive Eruptions
Hot fragments and volcanic ash which refer to sand or smaller fragments
Pyroclasts
Four-and-a-half billion years ago. Earth formed from a cloud of gas and dust in space. Solid particles, called “planetesimals” condensed out of the cloud. They’re thought to have stuck together and created the early Earth. Bombarding planetesimals heated Earth to a molten state.
- The Earth was formed by the process of accretion a portion of the original heat was trapped inside the Earth’s crust and has not yet been lost.
- Meteoroids attracted each other and formed bigger masses. This process accumulated a lot of heat.
THREE MAIN REASONS WHY THE
INTERIOR OF EARTH IS VERY HOT
- The heat from when
the planet formed
- Frictional heating, caused by denser core material sinking to the center of the planet.
- Some of the heat in the middle layers of the interior are hot because the deeper core is cooling and releasing heat.
- Earth is cooling now – but very, very slowly. Earth is close to a steady temperature state. Over the past several billion years, it might have cooled a couple of hundred degrees. Earth keeps a nearly steady
temperature, because it makes heat in its interior.
THREE MAIN REASONS WHY THE
INTERIOR OF EARTH IS VERY HOT
- FRICTIONAL HEATING
- It involves the decomposing of natural radioactive elements inside Earth – like uranium. Uranium is a special kind of element because when it decays, heat is produced. It’s this heat that keeps Earth from cooling off completely.
- Without this process of radioactive decay, there would be fewer volcanoes and earthquakes – and less building of Earth’s vast mountain ranges. This process contributes more than half of the heat in the earth.
THREE MAIN REASONS WHY THE
INTERIOR OF EARTH IS VERY HOT
- RADIOACTIVE DECAY
is defined as the process by which magma get out through the crust and crystallizes as an intrusive igneous rock beneath the Earth’s surface. The name
plutonism references Pluto, the classical ruler.
Plutonism
When magma forces itself into cracks, breaks off pieces of rock, and then envelops
them, this is called stoping. The resulting fragments are called _______. It is a piece of rock trapped in another type of rock
xenoliths