Quartzofeldspathic Schist And Gneiss Interbedded With Mica Schist And Gneiss
Gneiss, schist & quartzite. about 4,000 to 541 million years old. 8 crags on this site have their map point on it.
What the map says
Contains thin beds of knotted mica schist and granule to pebble metaconglomerate
1:100,000 sheet: Colton, Roger B., 1976, U.S. Geological Survey Geologic Investigations Series I-855-G (8 crags). A contact line at that scale is about 100 m wide on the ground.
Served by Macrostrat (CC BY 4.0). The wording is the map's own, quoted as a fact about the mapped unit, not about any one wall.
Estes Park Valley
- The Monastery101 routes · Big Thompson Canyon · 7,842 ft · gneiss and schist (another source)
- Beige Tube Area / The Narrows80 routes and 7 boulder problems · Big Thompson Canyon · 5,462 ft · gneiss and schist (another source)
- Basic Training Wall8 routes · Big Thompson Canyon · 6,830 ft · gneiss and schist (another source)
- Salt Block Rock8 routes · Big Thompson Canyon · 6,607 ft · gneiss and schist (another source)
- Five Point to a Fist Crag3 routes · Big Thompson Canyon · 6,396 ft · gneiss and schist (another source)
- Erid Weatherin1 route · Big Thompson Canyon · 6,751 ft · gneiss and schist (another source)
- Kafka on the Shore Boulder1 boulder problem · Big Thompson Canyon · 6,365 ft · gneiss and schist (another source)