C925 Earth: Inside and Out

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Free C925 Earth: Inside and Out Questions

1. Which driving force of plate tectonics pulls the plate downward at subduction zones?
  • Ridge push
  • Mantle drag
  • Slab pull
  • Hotspot push

Explanation

Slab pull is the dominant force moving tectonic plates, accounting for about 70–80% of the total driving energy. As cold, dense oceanic lithosphere sinks into the mantle at subduction zones, its weight pulls the rest of the plate along behind it like a conveyor belt. This gravitational sinking of old, heavy slabs is far stronger than ridge push from elevated mid-ocean ridges or drag from underlying mantle convection.
2. Which type of plate boundary creates mid-ocean ridges and rift valleys?
  • Divergent
  • Convergent
  • Transform
  • Hotspot

Explanation

Mid-ocean ridges and rift valleys form where two tectonic plates move away from each other, allowing magma from the mantle to rise and create new oceanic crust. This process, known as seafloor spreading, is characteristic of divergent plate boundaries. Examples include the Mid-Atlantic Ridge and the East African Rift. The upward movement of hot mantle material causes the crust to thin and crack, producing the ridge or valley features visible on Earth’s surface and beneath the oceans.
3. Which zone contains groundwater that completely fills all pore spaces?
  • Zone of aeration
  • Water table
  • Zone of saturation
  • Aquifer

Explanation

The zone of saturation is the subsurface layer where every available pore space and crack in rock or sediment is completely filled with groundwater. Above it lies the zone of aeration, where pores contain both air and water, and the boundary between them is the water table. Water in the zone of saturation flows slowly under gravity and pressure, supplying wells and springs, and forms the reservoir for most of Earth’s accessible freshwater outside of surface bodies.
4. When groundwater percolating through fractures in basalt picks up dissolved silica from the surrounding rock and deposits it as concentric layers around a nucleus in cavities, forming rounded spheres with distinctive banding, which variety of chalcedony has been created by this slow precipitation process over thousands of years?
  • Jasper
  • Flint
  • Chert
  • Agate

Explanation

Agate forms when silica-rich solutions fill gas pockets or cracks in volcanic rocks and deposit successive layers of microcrystalline quartz, creating colorful banding. Each band reflects slight changes in temperature, pressure, or chemistry, producing the beautiful patterns prized by collectors worldwide.
5. What does the Richter scale actually measure?
  • Damage caused
  • Energy released
  • Wave amplitude on seismograms
  • Intensity felt by people

Explanation

The Richter scale, developed in 1935, measures the maximum amplitude of seismic waves recorded on a specific type of seismograph corrected for distance. Each whole number increase represents a tenfold increase in amplitude and roughly 31 times more energy released. While modern scales like moment magnitude (Mw) are preferred for large earthquakes, the Richter scale remains widely understood as a quick estimate of an earthquake’s size based on wave amplitude.
6. Which metamorphic rock is formed from pure quartz sandstone?
  • Marble
  • Slate
  • Quartzite
  • Phyllite

Explanation

Quartzite forms when sandstone composed almost entirely of quartz grains is subjected to high heat and pressure, causing the grains to recrystallize and fuse into an extremely hard, non-foliated rock. The resulting quartzite is so durable that it often preserves original sandstone bedding as ghost-like cross-bedding and is prized as a building stone.
7. Where is the earthquake’s focus located?
  • On the surface directly above the rupture
  • At the point where the fault first breaks underground
  • At the seismograph station
  • Along the entire fault plane

Explanation

The focus, or hypocenter, is the exact point within Earth where seismic energy is first released as the fault suddenly slips and rocks break. It marks the origin of the earthquake deep underground, often tens to hundreds of kilometers below the surface. The point directly above the focus on the Earth’s surface is called the epicenter, which is what news reports typically reference when locating an earthquake.
8. In a region of active continental rifting where the crust is being stretched and thinned over millions of years, creating a series of stepped fault blocks that form alternating mountain ranges and sediment-filled basins, which specific type of fault dominates the landscape and has the hanging wall consistently dropping downward relative to the footwall along steeply dipping planes?
  • Reverse fault
  • Thrust fault
  • Strike-slip fault
  • Normal fault

Explanation

Normal faults dominate extensional tectonic settings where the lithosphere is pulled apart, allowing the hanging wall to collapse downward under gravity along faults dipping 50–70°. This process creates horst (uplifted blocks) and graben (down-dropped basins) topography, most spectacularly seen in the Basin and Range Province of the western United States and the East African Rift, where continued stretching will eventually split the continent and form a new ocean basin.
9. Which boundary marks the division between the mantle and outer core?
  • Moho
  • Conrad
  • Gutenberg discontinuity
  • Lehmann discontinuity

Explanation

The Gutenberg discontinuity is the seismic boundary approximately 2,900 km deep where the solid mantle ends and the liquid outer core begins. Here, P-wave velocity drops sharply and S-waves disappear entirely, proving the outer core is molten. Named after seismologist Beno Gutenberg, this boundary plays a crucial role in understanding Earth’s internal heat engine and magnetic field generation.
10. Which mountain range formed primarily by continent-continent collision?
  • Andes
  • Mid-Atlantic Ridge
  • Himalayas
  • Rockies

Explanation

The Himalayas formed when the Indian Plate collided with the Eurasian Plate about 50 million years ago, crumpling and uplifting ancient seafloor sediments into the world’s highest peaks. Ongoing convergence continues to raise Mount Everest by several millimeters annually.

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