| Intrusive Suite of Merced Peak | |
|---|---|
| Stratigraphic range: mid-Cretaceous, | |
| Type | Suite |
| Lithology | |
| Primary | Granodiorite |
| Location | |
| Region | Yosemite National Park |
| Country | United States |
| Type section | |
| Named for | Merced Peak |
 The Intrusive Suite of Merced Peak, near Merced Peak, lower right | |
The Intrusive Suite of Merced Peak is one of several intrusive suites in Yosemite National Park. These also include:
- Fine Gold Intrusive Suite
- Intrusive Suite of Buena Vista Crest
- Intrusive Suite of Jack Main Canyon
- Intrusive Suite of Sonora Pass
- Intrusive Suite of Yosemite Valley
- Johnson Granite Porphyry
- Tuolumne Intrusive Suite
Geology
The Intrusive Suite of Merced Peak dates to roughly 98 Ma. [1] The formation dates to mid-Cretaceous. It lies within the volcanogenic Minarets sequence, and comprises the granodiorite of Jackass Lakes and the leucogranites of Timber Knob and Norris Creek. Most of the suite is the former. [2]
See also
References
- ^ "Formation of the Yosemite Creek Granodiorite: a Field and Geochemical Study".
- ^ Bateman, Paul C. "U.S. GEOLOGICAL SURVEY" (PDF).
External links
 | This article about a specific United States geological feature is a stub. You can help Wikipedia by expanding it. |
| Intrusive Suite of Merced Peak | |
|---|---|
| Stratigraphic range: mid-Cretaceous, | |
| Type | Suite |
| Lithology | |
| Primary | Granodiorite |
| Location | |
| Region | Yosemite National Park |
| Country | United States |
| Type section | |
| Named for | Merced Peak |
|
The Intrusive Suite of Merced Peak, near Merced Peak, lower right | |
The Intrusive Suite of Merced Peak is one of several intrusive suites in Yosemite National Park. These also include:
- Fine Gold Intrusive Suite
- Intrusive Suite of Buena Vista Crest
- Intrusive Suite of Jack Main Canyon
- Intrusive Suite of Sonora Pass
- Intrusive Suite of Yosemite Valley
- Johnson Granite Porphyry
- Tuolumne Intrusive Suite
Geology
The Intrusive Suite of Merced Peak dates to roughly 98 Ma. [1] The formation dates to mid-Cretaceous. It lies within the volcanogenic Minarets sequence, and comprises the granodiorite of Jackass Lakes and the leucogranites of Timber Knob and Norris Creek. Most of the suite is the former. [2]
See also
References
- ^ "Formation of the Yosemite Creek Granodiorite: a Field and Geochemical Study".
- ^ Bateman, Paul C. "U.S. GEOLOGICAL SURVEY" (PDF).
External links
|
| This article about a specific United States geological feature is a stub. You can help Wikipedia by expanding it. |