Convergent

Divergent

Transform

Subduction

Sand, silt, clay, and organic matter

Sand, gravel, rocks, and minerals

Water, air, minerals, and rocks

Clay, pebbles, minerals, and organic matter

Soil composition affects the color of plants.

Soil composition determines the amount of sunlight plants receive.

Soil composition influences water retention and nutrient availability for plants.

Soil composition has no effect on plant growth.

The process of soil erosion

The change in shape or size of rocks due to stress

The movement of tectonic plates

The formation of new minerals

Stress causes rocks to melt, leading to volcanic eruptions.

Stress builds up in rocks until it is released as seismic energy, causing earthquakes.

Stress causes rocks to expand, creating new landforms.

Stress has no effect on earthquakes.

Stress is the force applied, while strain is the deformation resulting from stress.

Stress is the deformation, while strain is the force applied.

Stress and strain are the same.

Stress is a type of rock, while strain is a type of soil.

The process of mountain formation

The equilibrium between Earth's crust and mantle

The movement of tectonic plates

The erosion of soil

Through the melting of glaciers

By the erosion of mountains

By the redistribution of mass on Earth's surface, causing the crust to rise or sink

Through volcanic eruptions

Plate tectonics have no impact on mountain formation.

Mountain ranges form only due to volcanic activity.

Convergent plate boundaries can push crustal material upward, forming mountain ranges.

Mountain ranges form due to erosion of the Earth's surface.

Increased stress will have no effect on the fault line.

Increased stress may lead to the fault line becoming inactive.

Increased stress can lead to a higher likelihood of earthquakes along the fault line.

Increased stress will cause the fault line to disappear.

Soil composition has no role in preventing erosion.

Soils with high clay content are more prone to erosion.

Soils with a balanced composition of sand, silt, and clay can better resist erosion.

Only sandy soils can prevent erosion.

Isostasy explains that the crust is denser than the mantle, causing it to float.

Isostasy describes the crust as floating on the denser, more fluid mantle due to differences in density.

Isostasy states that the crust is immobile and does not float.

Isostasy is unrelated to the buoyancy of the crust.

Strain causes rocks to break apart, preventing folds.

Strain results in the bending and folding of rock layers under compressive stress.

Strain has no effect on rock layers.

Strain only affects the color of rock layers.

Convection currents in the mantle

Magnetic fields

Gravitational pull from the moon

Wind and ocean currents

They result in the subduction of one plate beneath another

They have no effect on the Earth's surface

They cause the formation of mountain ranges

They lead to the creation of new oceanic crust

Water only affects soil erosion in desert regions

Water can transport soil particles, leading to erosion

Water helps to compact soil, preventing erosion

Water has no impact on soil erosion

The lithosphere is the source of all volcanic activity.

The lithosphere is the rigid outer layer of Earth that includes tectonic plates.

The lithosphere is a liquid layer beneath the crust.

The lithosphere has no role in plate tectonics.

All soil textures retain the same amount of water.

Coarse-textured soils retain more water than fine-textured soils.

Soil texture has no effect on water retention.

Fine-textured soils, like clay, retain more water than sandy soils.

Convection currents in the mantle are responsible for the movement of tectonic plates.

Convection currents in the mantle are responsible for the formation of the atmosphere.

Convection currents in the mantle have no effect on the Earth's surface.

Convection currents in the mantle cause the Earth's rotation.