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Volcanoes
is a vent or opening in the Earth’s crust. Molten rock (magma), ash, and gases rise from underground. When pressure builds up, it may erupt onto the surface
lava
The released molten rock on the surface
ACTIVE VOLCANO
This type of volcano is always in the state of frequent eruptions and has erupted within the last 10,000 years.
Dormant Volcano
This type of volcano can erupt in the near future but may not have erupted for quite some time. Generally, these volcanoes may be regarded as semi-active volcanoes because they can erupt not as regularly or as frequently as active volcanoes.
EXTINCT VOLCANO
This type of volcano is expected not to erupt again and has not erupted in the past 10,000 years.
Island Arc, Hot spots, Spreading Center, Continental arc
4 ways volcanoes are formed
ISland Arc
Are long chains of active volcanoes with intense seismic activity found along convergent tectonic plate boundaries. most of these originate on oceanic crust and have resulted from the descent of the lithosphere into the mantle along the subduction zone. They are the principal way by which continental growth is achieved
Hot spots
form when a static plume of exceptionally hot magma rises from deep within the Earth's mantle to melt through the moving tectonic plate above it. Unlike most volcanoes, these do not occur at plate boundaries but instead erupt in the middle of tectonic plates.
Spreading Centers
Volcanoes form through decompression melting caused by tectonic plates pulling apart. This process occurs at divergent plate boundaries, where the Earth's crust thins, allowing magma from the mantle to rise and erupt onto the seafloor or land surface.
Continental Arc
form when an oceanic tectonic plate subducts beneath a continental tectonic plate, creating a line of volcanoes on the continental surface.
fault line
refers to a crack in the crust that is created when Earth’s crust shifts. When the sides of a fault move past each other, they generate seismic waves that create earthquakes
Western, Eastern, Central, Marikina valley, Southern Mindanao
5 Philippine faults
Western Philippine Fault
This fault line does not actually pass on land but across the seas found in the region of the country, which includes the Luzon Sea, Mindoro Strait, Panay Gulf, and Sulu Sea.
Eastern Philippine Fault
A major offshore fault line located in the Philippine Sea, that contributes to the country's earthquake activity.
Central Philippine Fault
A major fault zone that stretches across several provinces in the central Philippines. It is an active tectonic fault capable of generating strong earthquakes and plays a significant role in the country's seismic activity.
Marikina Valley Fault System
A major active fault system that runs through parts of Metro Manila and nearby provinces. It consists of the West Valley Fault and East Valley Fault and is capable of generating strong earthquakes that could significantly affect densely populated areas.
Southern Mindanao Fault
It runs through several provinces and is capable of generating strong earthquakes, posing a significant seismic hazard to nearby communities.
SPACE GEODETIC
SATELLITE-BASED METHODS USED TO ACCURATELY MEASURE THE EARTH'S SHAPE, POSITION, AND MOVEMENT. THEY HELP SCIENTISTS MONITOR TECTONIC PLATE MOVEMENTS, FAULT LINES, EARTHQUAKES, AND CHANGES IN THE EARTH'S SURFACE.
GLOBAL POSITIONING SYSTEM
THIS IS A NAVIGATION NETWORK OF SATELLITES ORBITING EARTH. these STATIONS, WHICH ARE USED FOR GEODESY, ARE LOCATED ON THE GROUND. WHEN MOVEMENTS OCCUR ON THE SURFACE OF EARTH, THE LOCATIONS OF THESE STATIONS ARE COMPARED WITH THEIR ORIGINAL LOCATIONS. SCIENTISTS CAN ALSO DETERMINE THE MOTION OF TECTONIC PLATES AND DEFORMATIONS ON EARTH'S CRUST. BY COMPARING THE LOCATIONS OF STATIONS ON DIFFERENT PLATES, SCIENTISTS CAN DETERMINE THE RATE AT WHICH THE PLATES MOVE.
VERY LONG BASELINE INTERFEROMETRY
THIS IS A HIGH-QUALITY RESOLUTION TECHNOLOGY THAT IS THE MOST SENSITIVE IN RECEIVING RADIO SIGNALS FROM SPACE. THIS MAKES USE OF AN ARRAY OF TELESCOPES THAT ARE COORDINATED FROM FAR DISTANCES. THE SIGNALS RECEIVED AT EACH TELESCOPE ARE THEN RECORDED TO BE PROCESSED AT A CORRELATION FACILITY.
SATELLITE LASER RANGING
USES POWERFUL LASERS TO MEASURE A SATELLITE'S POSITION BY DETECTING CHANGES FROM ITS PREDICTED ORBIT. IT ACCURATELY DETERMINES CHANGES IN THE EARTH'S CENTER OF MASS (GEOCENTER), HELPING ESTABLISH PRECISE GEODETIC INFRASTRUCTURE AND MONITOR THE EARTH. WORLDWIDE, THERE ARE ABOUT 42 SLR STATIONS, WITH ONLY 6 LOCATED IN THE SOUTHERN HEMISPHERE.
Hydrosphere, lithosphere, atmosphere
three spheres of the earth
crust
very thin layer of solid, thinnest layer
plates
the crust of the earth is broken into many pieces called ___, they also cause earthquakes when these ___ move.
continental crust
Thicker layer of the earths crust, its thick but less dense and 35km thick
oceanic crust
Thinner layer of the crust, under the ocean basin, denser and heavier and 7km thick only
Lithosphere 100km
composed of the crust and upper mantle, state how many km.
mohorovicic discontinuity
The boundary between the crust and the mantle
convection current
driven by heat from the core, magma rises cools and sinks to create a cycle.
continental drift, earthquakes and volcanic activity
The convection current drives plate tectonics which cause ___
asthenosphere
Made of molten rock and metal, so it flows like hot asphalt and is inside the upper mantle that moves and causes tectonic plates to move
Mantle, 2900km
largest layer of the earth, around ___ thick. it very flexible and flows like a viscous liquid.
1600f - 4000f
heat of the mantle
gutenberg discontinutity
boundary between the mantle and the core, found 2900km below the earths surfafce which checks out
Core
like a ball off very hot metal.
2200km, 4000c - 5500c
Outer core’s thickness and heat
1220km, 5400c - 5500c
inner core’s thickness and heat
convergent, divergent, transform
three plate boundaries
convergent
When plates move toards eachtoher, earthquakes and volcanoes happen.
subduction
In Convergent boundaries, one of the two plates is descending beneath the other. This process is called
Oceanic to Oceanic
an older plate is colder so its less bouyant so it subducts under the more younger, hotter and bouyant plate. deep oceanic trenches happen
oceanic to continental
the denser water subducts under the less dense land plate which causes a deep ocean trench and a line of volcanoes
continental to continental
no subduction happens since theyre both light and like two colliding icebergs they resist downawrd motions and just slam into eachother forming mountains and mountain ranges
divergent
occur when two tectonic plates move away from each other.
new crust
When two lithospheric plates are spread apart, it is common for _____ to form as molten material rises to the surface. The Mid-Atlantic Ridge is formed in this process.
transform
grind past each other without going up or down. capable of triggering devastating earthquakes. A famous example is the San Andreas Fault in California.
FOCUS / HYPOCENTER
where earthquake begins underground
EPICENTER
point on earth's surface directly above it