Caves

Limestone caves, lava tubes, stalactites, groundwater, cave ecosystems, and exploration.

Visual learning: These pages use real Wikimedia Commons scientific diagrams, geology photographs, landforms, and glacier imagery.
Earth Layers
Earth LayersA cutaway diagram helps show crust, mantle, outer core, and inner core.
Plate Boundaries
Plate BoundariesGlobal maps reveal major tectonic plates and their boundaries.
Grand Canyon
Grand CanyonLayered rock records long periods of deposition, uplift, and erosion.
Glacier
GlacierGlaciers shape valleys and store large amounts of freshwater ice.

Limestone Caves

Explore the key ideas behind limestone caves.

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Groundwater

Explore the key ideas behind groundwater.

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Stalactites

Explore the key ideas behind stalactites.

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Stalagmites

Explore the key ideas behind stalagmites.

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Lava Tubes

Explore the key ideas behind lava tubes.

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Cave Ecosystems

Explore the key ideas behind cave ecosystems.

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Cave Mapping

Explore the key ideas behind cave mapping.

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Cave Conservation

Explore the key ideas behind cave conservation.

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Limestone Caves

Limestone Caves is one part of the larger Earth system. Earth scientists compare rocks, landforms, maps, measurements, fossils, satellite observations, and field evidence to understand how this topic formed and how it changes over time. Studying limestone caves also shows how slow geologic processes can build dramatic landscapes over thousands to millions of years. Weather, water, ice, gravity, heat from inside Earth, and plate movement often work together rather than acting separately.

Groundwater

Groundwater is one part of the larger Earth system. Earth scientists compare rocks, landforms, maps, measurements, fossils, satellite observations, and field evidence to understand how this topic formed and how it changes over time. Studying groundwater also shows how slow geologic processes can build dramatic landscapes over thousands to millions of years. Weather, water, ice, gravity, heat from inside Earth, and plate movement often work together rather than acting separately.

Stalactites

Stalactites is one part of the larger Earth system. Earth scientists compare rocks, landforms, maps, measurements, fossils, satellite observations, and field evidence to understand how this topic formed and how it changes over time. Studying stalactites also shows how slow geologic processes can build dramatic landscapes over thousands to millions of years. Weather, water, ice, gravity, heat from inside Earth, and plate movement often work together rather than acting separately.

Stalagmites

Stalagmites is one part of the larger Earth system. Earth scientists compare rocks, landforms, maps, measurements, fossils, satellite observations, and field evidence to understand how this topic formed and how it changes over time. Studying stalagmites also shows how slow geologic processes can build dramatic landscapes over thousands to millions of years. Weather, water, ice, gravity, heat from inside Earth, and plate movement often work together rather than acting separately.

Lava Tubes

Lava Tubes is one part of the larger Earth system. Earth scientists compare rocks, landforms, maps, measurements, fossils, satellite observations, and field evidence to understand how this topic formed and how it changes over time. Studying lava tubes also shows how slow geologic processes can build dramatic landscapes over thousands to millions of years. Weather, water, ice, gravity, heat from inside Earth, and plate movement often work together rather than acting separately.

Cave Ecosystems

Cave Ecosystems is one part of the larger Earth system. Earth scientists compare rocks, landforms, maps, measurements, fossils, satellite observations, and field evidence to understand how this topic formed and how it changes over time. Studying cave ecosystems also shows how slow geologic processes can build dramatic landscapes over thousands to millions of years. Weather, water, ice, gravity, heat from inside Earth, and plate movement often work together rather than acting separately.

Cave Mapping

Cave Mapping is one part of the larger Earth system. Earth scientists compare rocks, landforms, maps, measurements, fossils, satellite observations, and field evidence to understand how this topic formed and how it changes over time. Studying cave mapping also shows how slow geologic processes can build dramatic landscapes over thousands to millions of years. Weather, water, ice, gravity, heat from inside Earth, and plate movement often work together rather than acting separately.

Cave Conservation

Cave Conservation is one part of the larger Earth system. Earth scientists compare rocks, landforms, maps, measurements, fossils, satellite observations, and field evidence to understand how this topic formed and how it changes over time. Studying cave conservation also shows how slow geologic processes can build dramatic landscapes over thousands to millions of years. Weather, water, ice, gravity, heat from inside Earth, and plate movement often work together rather than acting separately.