Grade 10 Science - 1st Mid-Quarter Examination Reviewer

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A comprehensive set of vocabulary flashcards covering Earth's layers, volcanic activity, earthquake dynamics, and the evolution of tectonic theories based on the Grade 10 Science Reviewer.

Last updated 8:10 AM on 8/4/26
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42 Terms

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Crust

The outermost and thinnest layer of the Earth, consisting of continental crust (3070km30\text{--}70\,km thick) and oceanic crust (510km5\text{--}10\,km thick).

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Granite

The main rock type that composes the continental crust.

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Basalt

The main rock type that composes the oceanic crust.

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Mantle

The thickest layer of the Earth, approximately 2,900km2,900\,km thick, composed of silicate rocks rich in magnesium and iron.

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Outer Core

A layer composed of liquid iron and nickel that is responsible for generating the Earth's magnetic field.

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Inner Core

The hottest layer of the Earth, made of solid iron and nickel due to extremely high pressure.

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Lithosphere

The layer consisting of the crust and the uppermost mantle, broken into tectonic plates.

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Asthenosphere

The soft, semi-fluid layer beneath the lithosphere that allows tectonic plates to move.

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Mesosphere

Technically defined in the text as the boundary between the outer core and the lower mantle.

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Magma Chamber

A reservoir that stores molten rock beneath the Earth's surface.

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Conduit

The underground passage through which magma travels to the surface.

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Dike

A vertical sheet of solidified magma that cuts across rock layers.

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Sill

A horizontal sheet of solidified magma between rock layers.

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Shield Volcano

A broad volcano with gentle slopes formed by fluid basaltic lava; an example is Mount Apo.

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Composite (Stratovolcano)

A tall, steep volcano with alternating layers of lava and ash that produces explosive eruptions, such as Mayon or Pinatubo.

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Cinder Cone

A small, steep volcano built from cinders and volcanic fragments, like Smith Volcano.

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Lava Dome

A rounded, slow-growing volcanic feature formed from thick, sticky lava.

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Plinian Eruption

A very explosive eruption style that produces tall eruption columns.

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Phreatic Eruption

A steam-driven explosion where no new magma reaches the surface.

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Phreatomagmatic Eruption

An explosion caused by the interaction of magma and water.

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Pyroclastic Flow

An extremely hot and fast-moving mixture of ash, rocks, and gases.

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Lahar

A volcanic mudflow composed of a mixture of ash, rocks, and water.

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Focus (Hypocenter)

The point inside the Earth where an earthquake begins.

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Epicenter

The point on the Earth's surface directly above the focus.

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P-Waves

The fastest seismic waves that can travel through solids, liquids, and gases.

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S-Waves

Seismic waves that are slower than P-waves and can travel only through solids.

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Surface Waves

The slowest seismic waves which cause the greatest damage; examples include Love Waves and Rayleigh Waves.

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Magnitude

The measure of the amount of energy released during an earthquake.

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Normal Fault

A fault caused by tension where the hanging wall moves downward relative to the footwall.

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Reverse Fault

A fault caused by compression where the hanging wall moves upward relative to the footwall.

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Strike-Slip Fault

A fault caused by horizontal movement, categorized as right-lateral (dextral) or left-lateral (sinistral).

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Triangulation Method

A method used to locate an earthquake epicenter using data from three seismic stations.

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Ridge Push

A cause of plate movement where new crust formed at mid-ocean ridges pushes older crust away.

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Slab Pull

A cause of plate movement where dense oceanic crust sinks into the mantle, pulling the rest of the plate.

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Divergent Boundary

A plate boundary where plates move apart, producing rift valleys and mid-ocean ridges.

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Convergent Boundary

A plate boundary where plates move toward each other, producing volcanoes, mountain ranges, and ocean trenches.

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Transform Boundary

A plate boundary where plates slide past each other, producing faults and earthquakes like the San Andreas Fault.

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Continental Drift Theory

The theory proposed by Alfred Wegener in 1912 suggesting all continents were once joined as Pangaea.

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Seafloor Spreading Theory

The theory proposed by Harry Hess in 1962 stating new oceanic crust forms at mid-ocean ridges and older crust is recycled by subduction.

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Glonar Challenger

The vessel that sent a 6km6\,km pipe to the ocean floor to collect drilling samples to support seafloor spreading.

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Magnetic Stripes

Alternating bands of magnetic polarity on both sides of mid-ocean ridges used as evidence for seafloor spreading.

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Plate Tectonic Theory

A unifying theory developed by several scientists that combines Continental Drift and Seafloor Spreading.