Rock Identifier
Rhyolite (Rhyolite (High-silica volcanic rock)) — igneous
igneous

Rhyolite

Rhyolite (High-silica volcanic rock)

Hardness: 6-7 on Mohs scale; Color: Reddish-brown, pink, or gray; Luster: Dull/Earthy to Sub-glassy; Crystal structure: Aphanitic (fine-grained) or Porphyritic; Cleavage: None/Irregular fracture; Specific gravity: 2.4-2.6.

Hardness
6-7 on Mohs scale
Color
Reddish-brown, pink, or gray
Luster
Dull/Earthy to Sub-glassy
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Reddish-brown, pink, or gray; Luster: Dull/Earthy to Sub-glassy; Crystal structure: Aphanitic (fine-grained) or Porphyritic; Cleavage: None/Irregular fracture; Specific gravity: 2.4-2.6.

Formation & geological history

Formed through the rapid cooling of high-silica (felsic) magma at or near the Earth's surface. This specimen appears to be from a volcanic flow or tuff deposit and can range in age from Recent to hundreds of millions of years old.

Uses & applications

Used in construction as crushed stone or road fill. Occasionally used as decorative stone in landscaping or for making stone tools (historically). Higher-grade or patterned versions (like Bird's Eye Rhyolite) are used in jewelry.

Geological facts

Rhyolite is the volcanic equivalent of granite. Because of its high silica content, rhyolitic lava is extremely viscous and can lead to explosive volcanic eruptions rather than flowing like basalt.

Field identification & locations

Identify by its light-to-reddish color, fine-grained texture, and high hardness (it will scratch glass). It is commonly found in continental volcanic regions such as the American Southwest and the Rocky Mountains.