| Structure | Orientation | Distinguishing Feature |
|---|---|---|
| Batholith | Deep large dome | Massive intrusion extending hundreds of square kilometers |
| Sill | Near horizontal sheet | Intrudes parallel between existing rock layers |
| Dike | Near vertical sheet | Cools in vertical cracks cutting across rock layers |
When you use it
Use when identifying landforms produced by magma cooling and solidifying beneath the surface.
Watch out
Sills lie parallel and horizontal between rock strata, while dikes cut vertically across existing layers.
Drafted from Grade 12 Geography, pages 2-34, then checked twice before it went up