| Filed | Form | Description | |
|---|---|---|---|
| 7/2/25 | DEF 14A | DEFINITIVE PROXY | → |
| 7/15/24 | DEF 14A | DEF 14A | → |
| 7/5/24 | PRE 14A | PRELIMINARY PROXY | → |
| 1/25/24 | DEF 14A | DEF 14A | → |
| 1/12/24 | PRE 14A | PRE 14A | → |
| 4/14/23 | DEF 14A | DEFINITIVE PROXY STATEMENT | → |
| ↓ | |||
| Filed | Form | Description | |
|---|---|---|---|
| 1/26/26 | 4 | 4 | → |
| 1/26/26 | 4 | 4 | → |
| 1/12/26 | 4 | 4 | → |
| 1/12/26 | 4 | 4 | → |
| 12/4/25 | 4 | 4 | → |
| 8/21/25 | 4 | 4 | → |
| ↓ | |||
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.