earth's geological processes & hazards (#3)

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63 Terms

1
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exogenic processes

these are external forces that operate and act on the Earth’s surface;

“destructive forces”

  • ex. weathering, mass wasting, soil erosion

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weathering

EXOGENIC PROCESSES:
refers to breaking down of rocks & minerals near the Earth’s surface;

can be physical, chemical, or biological

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physical weathering

TYPES OF WEATHERING:

process of rock & mineral breakdown without altering their chemical composition;

causes: water, wind, gravity, temperature change

<p><strong>TYPES OF WEATHERING:</strong></p><p>process of <strong>rock &amp; mineral breakdown without altering their chemical composition</strong>;</p><p>causes: water, wind, gravity, temperature change</p>
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chemical weathering

TYPES OF WEATHERING:

process of rock & mineral breakdown due to chemical reactions;

causes: elements, mineral composition, acids

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biological weathering

TYPES OF WEATHERING:

process of rock & mineral breakdown as a result of plant & animal activity;

causes: organisms

<p><strong>TYPES OF WEATHERING:</strong></p><p>process of rock &amp; mineral breakdown as a <strong>result of plant &amp; animal activity;</strong></p><p>causes: organisms</p>
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mass wasting

EXOGENIC PROCESSSES:

refers to the movement of rock and/or soil down a slope influenced by gravity;

  • ex. creep, debris flow, falls, slumps, solifluction

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creep

TYPES OF MASS WASTING:

slow and gradual movement of soil and rocks down a slope;

barely noticeable due to its very slow movement

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debris flow

TYPES OF MASS WASTING:

refers to the material flow caused by rainfall or seismic activity

<p><strong>TYPES OF MASS WASTING:</strong></p><p>refers to the<strong> material flow</strong> caused by <strong>rainfall or seismic activity</strong></p>
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falls

TYPES OF MASS WASTING:

occur when rocks or rock masses rapidly move down a slope

<p><strong>TYPES OF MASS WASTING:</strong></p><p>occur when <strong>rocks or rock masses rapidly move</strong> down a slope</p>
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slumps

TYPES OF MASS WASTING:

occur when soil and/or rock debris move downhill along a curved plane in a rotational manner

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solifluction

TYPES OF MASS WASTING:

sluggish flow of saturated soil down a slope related to freeze-thaw activity

<p><strong>TYPES OF MASS WASTING:</strong></p><p><strong>sluggish flow of saturated soi</strong>l down a slope related to <strong>freeze-thaw activity</strong></p>
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soil erosion

EXOGENIC PROCESSES:
gradual wearing away of the soil’s surface;

  • water erosion, wind erosion, gravitational erosion

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water erosion

TYPES OF EROSION:

degradation of soil due to flow of water from nearby bodies of water

<p><strong>TYPES OF EROSION:</strong></p><p>degradation of soil due to<strong> flow of water from nearby bodies of water</strong></p>
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wind erosion

TYPES OF EROSION:

natural process that moves soil from one place to another by wind power

<p><strong>TYPES OF EROSION:</strong></p><p>natural process that moves<strong> soil from one place to another by wind power</strong></p>
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gravitational erosion

TYPES OF EROSION:

erosion wherein rocks & sediments move under gravity’s influence

<p><strong>TYPES OF EROSION:</strong></p><p>erosion wherein rocks &amp; sediments move under gravity’s influence</p>
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True

TRUE OR FALSE:

In erosion, nutrient depletion in the soil could be observed due to the loss of minerals.

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True

TRUE OR FALSE:

In erosion, issues regarding water purity arise as eroded sediments become mixed with water.

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endogenic processes

these are internal forces that exist deep inside the Earth

  • ex. tectonic plates, faults, earthquakes, volcanoes

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plate tectonics theory

though it remains a theory, this aims to explain how major landforms are created as a result of Earth’s subterranean movements

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tectonic forces

ENDOGENIC FORCES:

these refer to the energy that causes a change in the Earth’s crust

  • compressional, tensional, & shear stress (CTS)

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compressional stress

3 TYPES OF STRESS:

occurs when tectonic plates are pushed together, resulting in a shorter but thicker crust

  • ex. Sierra Madre

<p><strong>3 TYPES OF STRESS:</strong></p><p>occurs when <strong>tectonic plates are pushed together</strong>, resulting in a <strong>shorter but thicker crust</strong></p><ul><li><p>ex. Sierra Madre</p></li></ul><p></p>
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tensional stress

3 TYPES OF STRESS:

occurs when tectonic plates are pulled apart, resulting in a thinner crust

  • ex. East African Rift (or rift valleys in general)

<p><strong>3 TYPES OF STRESS:</strong></p><p>occurs when tectonic plates are <strong>pulled apart</strong>, resulting in a thinner crust</p><ul><li><p>ex. East African Rift (or rift valleys in general)</p></li></ul><p></p>
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shear stress

3 TYPES OF STRESS:

occurs when parallel plates move in opposite directions, commonly leading to formation of faults

  • ex. San Andreas Fault

<p><strong>3 TYPES OF STRESS:</strong></p><p>occurs when<strong> parallel plates move in opposite directions</strong>, commonly leading to <strong>formation of faults</strong></p><ul><li><p>ex. San Andreas Fault</p></li></ul><p></p>
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fault

ENDOGENIC PROCESSES:

refers to the fracture or zone of fractures between two blocks of rocks or 2 tectonic plates

  • normal, reverse, strike-slip (NRS)

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normal fault

3 TYPES OF FAULT:

this forms when the Earth’s surface moves apart due to tensional stress;

<p><strong>3 TYPES OF FAULT:</strong></p><p>this forms when the Earth’s surface moves apart due to <strong>tensional stress;</strong></p><p></p>
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normal fault

3 TYPES OF FAULT:

this occurs when the hanging wall moves down relative to the foot wall

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reverse fault

3 TYPES OF FAULT:

this forms when the Earth’s surface moves towards one another & is associated with compressional stress

<p><strong>3 TYPES OF FAULT:</strong></p><p>this forms when the Earth’s surface moves towards one another &amp; is associated with <strong>compressional stress</strong></p>
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reverse fault

3 TYPES OF FAULT:
occurs when the hanging wall moves up or is thrust over the foot wall

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thrust fault

this a form of reverse fault in which the dip is less than 45 degrees

<p>this a form of reverse fault in which the dip is <strong>less than 45 degrees</strong></p>
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strike-slip fault (transcurrent fault)

3 TYPES OF FAULT:

this is formed due to the sideways movement of blocks/plates

  • can be right lateral strike-slip fault or left lateral strike-slip fault

<p><strong>3 TYPES OF FAULT:</strong></p><p>this is formed due to the<strong> sideways movement </strong>of blocks/plates</p><ul><li><p>can be right lateral strike-slip fault or left lateral strike-slip fault</p></li></ul><p></p>
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strike-slip fault (transcurrent fault)

3 TYPES OF FAULT:

in this fault, the block moves laterally in opposite directions relative to a reference point

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right lateral strike-slip fault and left lateral strike-slip fault

2 classification of strike-slip fault

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False; tsunamis should be earthquakes

TRUE OR FALSE:

Normal, reverse, and strike-slip faults result in tsunamis and the alteration of Earth’s crust.

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normal and reverse faults, strike-slip fault

What types of fault form these geographical formations?

  1. rifts, valleys, & mountains

  2. valleys or undersea canyons

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earthquakes

ENDOGENIC PROCESSES:

these are caused by the movement of tectonic plates due to tectonic forces;

also produce seismic waves;

seismograph is used to detect/record seismic waves

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seismic waves

ENDOGENIC PROCESSES:

these are vibrations that transmit energy & occur during seismic activities (like earthquakes, volcanic eruptions, & man-made explosions)

  • primary & secondary waves

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primary waves (p-waves/pressure waves)

these are longitudinal waves, which means that the direction of motion & propagation are the same

<p>these are<strong> longitudinal waves</strong>, which means that the direction of motion &amp; propagation are the same</p>
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secondary waves (s-waves)

these are transverse waves, which means that the motion is perpendicular to the direction of wave propagation

<p>these are <strong>transverse</strong> waves, which means that the <strong>motion is perpendicular to the direction of wave propagation</strong></p>
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subduction

ENDOGENIC PROCESSES:
volcanoes form from the process of _______, wherein either an oceanic plate descends below another oceanic plate or an oceanic plate descends under a continental plate

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shield volcano

TYPES OF VOLCANO:

this is shaped as a bowl with long gentle slopes made by basaltic lava flows;

formed by eruption of low-viscosity lava that can flow a great distance from a vent

  • ex. Mauna Kea (Hawaii)

<p><strong>TYPES OF VOLCANO:</strong></p><p>this is shaped as a bowl with <strong>long gentle slopes</strong> made by <strong>basaltic lava flows;</strong></p><p>formed by eruption of <strong>low-viscosity lava</strong> that can flow a great distance from a vent</p><ul><li><p>ex. Mauna Kea (Hawaii)</p></li></ul><p></p>
41
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stratovolcano (composite volcano)

TYPES OF VOLCANO:

is a steep-sided volcano composed of many layers of volcanic rocks, usually made from high-viscosity lava, ash, & rock debris

  • ex. Mount Mayon (Bicol)

<p><strong>TYPES OF VOLCANO:</strong></p><p>is a steep-sided volcano composed of many layers of volcanic rocks, usually made from <strong>high-viscosity lava,</strong> ash, &amp; rock debris</p><ul><li><p>ex. Mount Mayon (Bicol)</p></li></ul><p></p>
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cinder volcano

TYPES OF VOLCANO:

this is circular or oval made up of small fragment of lava from a single vent that have been flown up;

low-viscosity lava;

results from eruptions of mostly small pieces of scoria and pyroclastic that build up around the vent

  • ex. Smith Volcano (Babuyan Island)

<p><strong>TYPES OF VOLCANO:</strong></p><p>this is <strong>circular or oval made up of small fragment of lava from a single vent</strong> that have been flown up;</p><p><strong>low-viscosity lava;</strong></p><p>results from eruptions of mostly small pieces of scoria and pyroclastic that build up around the vent</p><ul><li><p>ex. Smith Volcano (Babuyan Island)</p></li></ul><p></p>
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magmatic eruptions

3 MAIN MECHANISMS OF VOLCANIC ERUPTIONS:
these are caused when gas releases under decompression

<p><strong>3 MAIN MECHANISMS OF VOLCANIC ERUPTIONS:</strong><br>these are caused when <strong>gas releases under decompression</strong></p>
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phreatic eruptions

3 MAIN MECHANISMS OF VOLCANIC ERUPTIONS:

these are caused when an ejection of entrained particles during steam eruptions happen

<p><strong>3 MAIN MECHANISMS OF VOLCANIC ERUPTIONS:</strong></p><p>these are caused when an ejection of <strong>entrained particles during steam eruptions happen</strong></p>
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phreatomagmatic eruptions

3 MAIN MECHANISMS OF VOLCANIC ERUPTIONS:

these are caused when a thermal contraction from chilling on contact with water happens

<p><strong>3 MAIN MECHANISMS OF VOLCANIC ERUPTIONS:</strong></p><p>these are caused when a <strong>thermal contraction from chilling on contact with water happens</strong></p>
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natural hazards

RS BETWEEN GEOLOGIC PROCESSES & NATURAL HAZARDS:

refer to natural events that threaten lives, property, and other assets;

both endogenic & exogenic influence the occurence of _______ _______

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tectonic hazards, geomorphological hazards, hydrometeorological hazards

3 TYPES OF NATURAL HAZARDS:

  1. during earthquakes & volcanic eruptions

  2. during landslides & soil erosion

  3. during storms & flooding

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cascading effect

RS BETWEEN GEOLOGIC PROCESSES & NATURAL HAZARDS:

this is a chain reaction where one geological event leads to multiple secondary consequences;

  • ex. volcanic eruptions causing climate change that leads to extreme weather; deforestation causes soil erosion and leads to landslides.

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feedback loop

RS BETWEEN GEOLOGIC PROCESSES & NATURAL HAZARDS:

this occurs when an initial geological process reinforces itself, either increasing or decreasing an event’s intensity

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positive feedback loop

TYPES OF FEEDBACK LOOP:

this relates to amplifying effects

  • ex. Glacial melting causing crustal rebound that leads to more earthquakes

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negative feedback loop

TYPES OF FEEDBACK LOOP:

this relates to stabilizing effects

  • ex. after a volcanic eruption volcanic, ash enriches the soil with minerals that lead to fertile lands encouraging plant growth that stabilizes the soil with vegetation that prevents further erosions

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geological processes

these shape Earth’s landscapes but also contribute to hazards like earthquakes, volcanic eruptions, landslides, and floods;

these interactions amplify hazard risks, making them harder to predict and control.

  • ex. Earthquake (endogenic) causing a landslide (exogenic) leading to a river blockage that causes flooding

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caldera

refers to the large depression formed when a volcano erupts and collapses;

during a volcanic eruption, magma present in the magma chamber underneath the volcano is expelled, often forcefully

<p>refers to the <strong>large depression formed when a volcano erupts and collapses</strong>;</p><p>during a volcanic eruption, magma present in the magma chamber underneath the volcano is expelled, often forcefully</p>
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Richter scale

UNDER EARTHQUAKES:

measures the strength/magnitude of earthquakes;

uses Arabic numbers (1 to 10), wherein magnitude 2 is 10x stronger than magnitude 1, & so on;

  • Moment magnitude scale (now more commonly used bc of higher precision)

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Mercalli scale

UNDER EARTHQUAKES:

intensity is measured using this (Roman numerals, I to X)

<p><strong>UNDER EARTHQUAKES:</strong></p><p>intensity is measured using this (Roman numerals, I to X)</p>
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focus/hypocenter

UNDER EARTHQUAKES:

earthquake’s point of origin inside the earth

<p><strong>UNDER EARTHQUAKES:</strong></p><p>earthquake’s point of origin inside the earth </p>
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epicenter

UNDER EARTHQUAKES:

point on earth’s surface directly above the focus

<p><strong>UNDER EARTHQUAKES:</strong></p><p>point on earth’s surface directly above the focus </p>
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magnitude, intensity

UNDER EARTHQUAKES:

  1. the size of an earthquake or energy released

  2. amount of damage caused by an earthquake

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Continental Drift Theory by Alfred Wegener (1912)

UNDER TECTONICS:

theory of the movement of the continents relative to each other;

some evidences are:

  • fossils in Africa & South America

  • positions of mountain ranges

  • glacial striations - scratches in rock caused by movement of glaciers

  • tillites - glacial sediments buried in rock

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tillites

refers to glacial sediments buried in rock

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Pangaea

UNDER PLATE TECTONICS:

the "supercontinent" that existed during the Paleozoic and Mesozoic eras; broke up into Laurasia in the north and Gondwanaland in the south during the Mesozoic era

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Laurasia

UNDER PLATE TECTONICS:

started breaking up into Asia, Europe, and North America during the Cenozoic era

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Gondwanaland

UNDER PLATE TECTONICS:

started breaking up into Africa, Australia, Antarctica, and South America during the Mesozoic era