John Day Formation
| John Day Strata Stratigraphic range: Oligocene, lower Miocene | |
|---|---|
 Exposures of the Turtle Cove Formation along a hiking trail in the Sheep Rock Unit of the John Day Fossil Beds National Monument | |
| Type | sedimentary (mostly from clasts of igneous origin), igneous |
| Underlies | Columbia River Basalt Group |
| Overlies | Clarno Formation |
| Lithology | |
| Primary | sandstone, tuff |
| Other | pyroclastic |
| Location | |
| Region | Central Oregon |
| Country | United States |
| Type section | |
| Named for | John Day River |
The John Day Formation is a series of rock strata exposed in the Picture Gorge district of the John Day River basin and elsewhere in north-central Oregon in the United States. The Picture Gorge exposure lies east of the Blue Mountain uplift, which cuts southwest–northeast through the Horse Heaven mining district northeast of Madras. Aside from the Picture Gorge district, which defines the type, the formation is visible on the surface in two other areas: another exposure is in the Warm Springs district west of the uplift, between it and the Cascade Range, and the third is along the south side of the Ochoco Mountains. All three exposures, consisting mainly of tuffaceous sediments and pyroclastic rock rich in silica, lie unconformably between the older rocks of the Clarno Formation below and Columbia River basalts above.[1]
The strata, which vary in age from 39 million years to 18 million years, were formed mainly from ashfalls from volcanoes to the west. Some of the major layers within the group exposed in the Picture Gorge district are the Big Basin Formation and Bridge Creek Beds (35 to 32 million years), the Turtle Cove Formation (30 to 28 million years), the Picture Gorge Ignimbrite (28.7 million years), the Kimberly Formation (28 to 25 million years), and the Haystack Formation (25 to 18 million years).[2]
Located in the general vicinity of what became the Cascade Range, the John Day volcanoes emitted large volumes of ash and dust, much of which settled in the John Day basin. The rapid deposition of the ash preserved the remains of plants and animals living in the region. Some of the solidified ash and the fossils they contain are found in the John Day Fossil Beds National Monument. Because ash and other debris fell during varied climatic and volcanic conditions and accumulated from many eruptions extending into the early Miocene (about 20 million years ago), the sediment layers in the fossil beds vary in their chemical composition and color.[3] The lowermost layer contains red ash, such as that exposed in the Painted Hills Unit of the national monument.[4] The layer above it is mainly pea-green clay. On top of the pea-green layer are buff-colored layers.[3]
Fossils found in the John Day Formation include a wide variety of plants and more than 100 species of mammals, including dogs, cats, oreodonts, horses, camels, and rodents.[5] Among the notable plant fossils are Metasequoia (Dawn Redwood), a genus thought to have gone extinct worldwide until it was discovered alive in China in the early twentieth century.[6]
References
- ↑ Woodburne, M.O.; Robinson,, P.T. (July 1977). "A New Late Hemingfordian Mammal Fauna from the John Day Formation, Oregon, and its Stratigraphic Implications". Journal of Paleontology. The Society of Economic Paleontologists and Mineralogists. 51 (4): 750–57. JSTOR 1303741. (subscription required (help)).
- ↑ "The Geologic Formations of the John Day Basin" (PDF). Oregon Paleo Lands Institute. Retrieved September 23, 2011.
- 1 2 Orr, pp. 30–31
- ↑ Orr, pp. 30–31, 46
- ↑ "Geology Fieldnotes". National Park Service. Retrieved July 25, 2011.
- ↑ Orr, p. 46
Works cited
- Orr, Elizabeth L., and Orr, William N. (1999). Geology of Oregon, 5th ed. Dubuque, Iowa: Kendall/Hunt Publishing Company. ISBN 0-7872-6608-6.
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