1/39
Section 1 – Structural Landforms (≈ 1 – 20) Batholith • Stock • Dike • Sill • Laccolith • Volcanic Neck • Breccia Neck • Exposures like Stone Mountain, Yosemite, Devils Tower, etc. Section 2 – Magma Composition & Texture (≈ 21 – 30) Phaneritic vs Aphanitic • Pegmatitic • Cooling rates • Depth vs crystal size • Relation to plutonic environments. Section 3 – Practice Quiz (Plutonic Focus) (≈ 31 – end) Only the questions in your PDF tied to intrusive/plutonic concepts (e.g., “Which texture forms from slow cooling?” “Where would you find a granite batholith exposed?”).
Name | Mastery | Learn | Test | Matching | Spaced |
|---|
No study sessions yet.
Batholith – Definition
A massive body of intrusive igneous rock that forms from cooled magma deep underground; exposed after erosion removes overlying layers.
Batholith – Size
Largest intrusive bodies; cover hundreds to thousands of square kilometers.
Batholith – Composition
Typically granitic (felsic); coarse-grained texture due to slow cooling.
Yosemite National Park, California – part of the Sierra Nevada Batholith.
A smaller version of a batholith (<100 km² exposed area); irregular shape.
Stone Mountain, Georgia – exposed granitic stock formed from slowly cooled magma.
A vertical or steeply inclined sheet of intrusive igneous rock that cuts across surrounding rock layers.
Forms when magma forces its way through fractures, cutting across preexisting rock layers.
Dikes in the Sierra Nevada and at Shiprock, New Mexico.
A tabular, sheetlike intrusion that runs parallel to existing rock layers.
Forms when magma intrudes between sedimentary layers without cutting across them.
Palisades Sill, New York – an example of mafic magma intrusion forming gabbro.
A lens-shaped pluton that forms when viscous magma pushes overlying strata upward.
Henry Mountains, Utah – laccolithic domes formed from magma intrusions.
Remnant of solidified magma within a volcano’s conduit after erosion removes the cone.
Devils Tower, Wyoming – columnar jointed phonolite plug.
A volcanic neck composed of broken angular rock fragments cemented by magma.
Shiprock, New Mexico – formed from fragmented volcanic materials around a neck.
Deep-seated plutons become visible only after millions of years of uplift and erosion expose them.
Reveal the interior architecture of ancient volcanoes and magma systems.
Coarse-grained texture where individual crystals are visible; forms from slow cooling of magma deep underground.
Granite, Diorite, Gabbro – all intrusive rocks.
Very coarse-grained igneous texture formed by slow cooling and abundant fluids near the end of crystallization.
Forms in late-stage crystallization zones within plutons; may contain rare minerals like tourmaline or beryl.
Slow cooling → large crystals (intrusive); fast cooling → small crystals (extrusive).
The deeper the magma cools, the slower the cooling rate and larger the crystal size.
Identified by coarse-grained (phaneritic) or pegmatitic texture.
As magma cools underground, early-formed minerals settle, creating layered plutonic bodies.
Felsic magmas form granite batholiths; mafic magmas form gabbroic intrusions.
Explains order of mineral formation; affects the composition and appearance of intrusive rocks.
Phaneritic or Pegmatitic texture.
Granite.
Dike cuts across layers (vertical); sill runs parallel to layers (horizontal).
A granitic stock.
Batholith.
A laccolith domes the overlying rock upward; a sill does not.
Erosion removes overlying layers, exposing deep intrusive bodies.
Phaneritic (coarse-grained).
Devils Tower, Wyoming.
Yosemite National Park, Sierra Nevada Batholith.