| Holder Formation | |
|---|---|
| Stratigraphic range: | |
| Type | Formation | 
| Underlies | Bursum Formation | 
| Overlies | Beeman Formation | 
| Thickness | 850 ft (260 m) | 
| Lithology | |
| Primary | Limestone | 
| Other | Shale | 
| Location | |
| Coordinates | 32°49′19″N105°52′26″W / 32.822°N 105.874°W | 
| Region | New Mexico | 
| Country | United States | 
| Type section | |
| Named for | Holder Ridge | 
| Named by | L.C. Pray | 
| Year defined | 1954 | 
The Holder Formation is a geologic formation in the Sacramento Mountains of New Mexico. It preserves fossils dating back to the late Pennsylvanian. [1]
The Holder Formation consists of limestone, red and gray calcareous shale, sandstone, and conglomerate. The maximum thickness is 850 ft (260 m). [1] The formation overlies the Beeman Formation [1] and is overlain by the Laborcita Formation. [2]
The formation is interpreted as a shallow-shelf marine formation of Virgilian (latest Pennsylvanian) age [3] during a global ice age. [4]
Bioherms are present at the base of the formation. [1] These are up to 50–75 feet (15–23 meters) thick. [3] They are composed of uncalcified cup-shaped phylloid (leaf-like [5] ) algae surrounded by masses of beresellid algae. [4]
The unit was first named by Lloyd C. Pray in 1954 [1] and a type section was designated in 1959. [6] Pray originally assigned the formation to the Magdalena Group, but the Magdalena Group has subsequently been abandoned. [3] [2]