| Filed | Description | |
|---|---|---|
| 6/12/25 | 1.01 Material Agreement | → |
| 6/12/25 | 1.02 Agreement Terminated | → |
| 3/17/25 | 1.01 Material Agreement | → |
| 1/7/25 | 1.01 Material Agreement | → |
| 4/23/24 | 1.01 Material Agreement | → |
| 4/5/24 | 1.01 Material Agreement | → |
| ↓ 11 more | ||
In geology, an igneous intrusion is a body of intrusive igneous rock that forms by crystallization of magma slowly cooling below the surface of the Earth. Intrusions have a wide variety of forms and compositions, illustrated by examples like the Palisades Sill of New York and New Jersey; the Henry Mountains of Utah; the Bushveld Igneous Complex of South Africa; Shiprock in New Mexico; the Ardnamurchan intrusion in Scotland; and the Sierra Nevada Batholith of California.