Plate Boundaries & Motions
Evidence & Data (GPS, Fossils, Seafloor, Continental Fit)
Rock Cycle & Energy Flow
Uplift, Weathering, and Erosion
Earthquakes & Seismicity
100

At divergent plate boundaries, plates:

  •  Move apart

100
  1. The direction of long‑term motion of Mt. Everest is:

Northeast

100

Sedimentary rock primarily forms from

  • Compaction and cementation of sediments

100
  1. Erosion transports sediment primarily by:

  • A) Water, wind, ice, and gravity

100
  1. The epicenter of an earthquake is:

  • he point on Earth’s surface directly above the focus

200
  1. Transform boundaries are characterized by plates that:

  • C) Slide past each other horizontally

200
  1. GPS stations help scientists:

  • B) Measure the rate and direction of plate motion

200

Metamorphic rock forms from:

  • Heat and pressure altering existing rock without melting

200
  1. An older layer is typically found:

Below younger layers

200
  1. The focus (hypocenter) of an earthquake is:

  • The point within the Earth where rupture starts

300

A typical surface feature at an oceanic divergent boundary is a:

  • Mid‑ocean ridge

300
  1. Seafloor age patterns indicate that:

  •  Crust is youngest near mid‑ocean ridges and older toward trenches

300
  1. Igneous rock forms from:

  • A) Cooling and solidification of magma or lava

300

Coastal cliffs retreat mainly due to:

  • Wave erosion and weathering

300
  1. Shallow earthquakes are most common at:

  • A) Divergent and transform boundaries

400
  1. Continental‑continental convergence most often produces:

  •  Large mountain ranges

400
  1. Earthquake epicenter patterns commonly align with:

  • Plate boundaries

400
  1. Seafloor spreading contributes to the rock cycle by:

  • Creating new igneous crust at ridges

400

DAILY DOUBLE: 

  1. A fossil exposed on a mountaintop without digging is explained by:

  • Uplift followed by erosion of overlying material

400
  1. The most common hazard from transform boundary quakes is:

  • Ground shaking and surface rupture

500
  1.  typical surface feature at an oceanic‑oceanic convergent boundary is a:

  • A) Deep ocean trench and island arc

500
  1. Fossils of marine organisms found on mountains suggest:

  • Uplift of formerly low‑lying or marine sediments

500
  1. Subduction contributes to the rock cycle by:

  • Driving metamorphism and generating magma

500

What is the difference between weathering and erosion?

Erosion involves deposition in a different location

500

DAILY DOUBLE

Earthquake magnitude measures:

  • Energy released during the quake

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