Ringold Formation

Ringold Formation
Stratigraphic range: Late Miocene-Pliocene, 8.5–3 Ma
The Columbia River flowing through the Ringold Formation.
TypeFormation
UnderliesDeposits from Missoula Floods
OverliesColumbia River Basalt Group
Thickness1,000 feet (300 m)
Location
Coordinates46°40′01″N 119°26′10″W / 46.667°N 119.436°W / 46.667; -119.436
RegionWashington (state)
CountryUnited States
Type section
Named forRingold Post Office
Named byJohn C. Merriam, John P. Buwalda

The Ringold Formation is a geological formation in Eastern Washington, United States. The formation consists of sediment laid down by the Columbia River following the flood basalt eruptions of the Columbia River Basalt Group, and reaches up to 1,000 feet (300 m) thick in places. It preserves fossils dating back to the late Miocene and Pliocene epochs of the Neogene period.

Exposures of the Ringold Formation can be found from Hanford Reach National Monument north to the Moses Lake area. Large portions of the formation are buried by other sediment deposits, extending as far as Wallula Gap southeast of Kennewick. In recent years, irrigation water entering the groundwater system has destabilized some Ringold Formation slopes and cliffs, causing landslides. The formation was named in 1917 for a school of the same name that existed at the time. Ringold School was located on the Franklin County side of the Columbia River to the south of Savage Island.

Geology

During the flood basalt eruptions before the sediments were laid down, the Columbia River followed a different route than it does today, taking it near the present-day sites of Yakima and Goldendale. North-to-south compression of the Columbia Plateau caused anticline folds like Rattlesnake Mountain and the Horse Heaven Hills to rise.

These ridges provided geographic barriers, rerouting the river eastward toward the Tri-Cities with it eventually flowing through Wallula Gap. During part of this period, the Columbia River was completely dammed leading to the development of a large lake covering the Yakima Valley and southern Columbia Basin. The Ringold Formation is the sediment laid down during the period of the lake's existence and while the route of the river was changing.

Some of the sediments found as part of the formation may have been sourced from ancestral versions of other Pacific Northwest rivers like the Clearwater and Pend Oreille. Layers of volcanic ash can also be found, with thicknesses ranging from being barely noticeable to 4 feet (1.2 m) thick.

Stratigraphy

The Ringold Formation represents sand and gravel placed by the Columbia River between around 8.5 and 3 million years ago. These deposits overlay cooled lava erupted as part of the Columbia River Basalt Group, a type of volcanic eruption known as flood basalts erupting from fissures across eastern Washington and Oregon that were unrelated to the Cascade Range. It is covered in places by deposits from the Missoula Floods.

Regional uplift caused the Columbia to erode parts of the Ringold Formation. The White Bluffs on Hanford Reach National Monument are a significant example of this.

Recent landslides

Sand dunes on top of White Bluffs. The material in this small dune field is from a nearby landslide.

Landslides along the Columbia River have increased in recent years due to irrigation around Basin City and Othello. Irrigation water enters and flows through the groundwater system toward the river easily through deposits left by the Missoula Floods. This destabilizes Ringold Formation features like the White Bluffs, causing the landslides. Landslides did not occur frequently before 1960. Rapid changes in river flow caused by the Priest Rapids Dam upstream may also contribute to slope destabilization.

The largest landslide in the White Bluffs portion of the formation is adjacent to Locke Island. This complex, initiated in the 1970s, has rerouted the Columbia River. As a result of the change, critical salmon spawning habitat has been destroyed. The landslide restricts the flow of the river on the east side of the river and as a result, large portions of Locke Island are being removed by the Columbia River. Movement of this landslide is ongoing, but the primary factor behind the continued movement is destabilization by the Columbia River eroding the fallen material. Blown sand from this landslide is the primary source material for sand dunes atop the bluffs near the island.

The Locke Island slide is the northernmost slide along the White Bluffs. There are at least five other major slides into the Columbia River, with the southernmost one being across the river from Pacific Northwest National Laboratory in north Richland, which occurred in 2008. At least one slide has occurred in nearby coulees.

Paleobiota

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon

Notes
Uncertain or tentative taxa are in small text
crossed out taxa are discredited.

Mammals

The mammal fossils of the Ringold Formation are divided into several local faunas, from youngest to oldest:

Artiodactyla

Artiodactyls of the Ringold Formation
Genus / Taxon Species Local fauna Notes Images
Antilocapridae White Bluffs Indeterminate pronghorns.
† Bretzia † B. pseudalces White Bluffs A very common capreoline deer with palmate antlers similar to moose. One of the earliest deer in North America.
† Camelops † C. sp. Taunton A large camel.
† Capromeryx † C. tauntonensis Taunton An antilocaprid (pronghorn). Later Capromeryx species were quite small, but this early species was only slightly smaller than living pronghorns.
Cervidae Blufftop, Taunton Indeterminate deer. Some Taunton fossils are similar to Odocoileus (mule deer and kin) and Rangifer (reindeer).
† Hemiauchenia † H. blancoensis White Bluffs, Taunton A common lamine camelid (related to llamas, alpacas, and kin).
† Megatylopus † M. sp. aff. M. gigas River Road,

White Bluffs

 A common large camel, either M. gigas or M. cochrani.
† Platygonus † P. pearcei White Bluffs A common flat-headed peccary.
† P. sp. Taunton

Carnivora

Carnivorans of the Ringold Formation
Genus / Taxon Species Local fauna Notes Images
Bassariscus B. astutus White Bluffs, Taunton The living ringtail, a species of procyonid (raccoon-like mammals).
† Borophagus † B. diversidens Taunton A very large borophagine (bone-crushing dog).
† B. hilli White Bluffs
† Buisnictis † B. cf. breviramus Taunton A skunk.
Canis † C. lepophagus Taunton A coyote-like canine.
† Chasmaporthetes † C. ossifragus White Bluffs A long-limbed hyena.
† Dinofelis cf. † D. paleoonca Taunton A possible machairodontine (saber-toothed cat).
† Eucyon † E. davisi White Bluffs A coyote-like canine, previously classified as a species of Canis.
"Felis" F. sp. White Bluffs, Taunton A cougar-sized cat, probably the same as Puma lacustris or "Lynx rexroadensis".
cf. † Homotherium cf. † H. sp. White Bluffs A relatively small machairodontine (saber-toothed cat).
† Huracan † H. cf. schneideri White Bluffs A large ailuropodine (panda-like) bear, previously considered a species of Agriotherium. One of the last surviving ailuropodine bears in North America.
Lynx L. cf. rufus Taunton A possible bobcat.
Mustela † M. cf. rexroadensis Taunton A weasel.
† Parailurus † P. sp. Taunton A large ailurid (red panda-like mammal).
† Plionarctos † P. harroldorum White Bluffs A tremarctine (short-faced bear) which was probably ancestral to later tremarctines. Fossils of this species were previously identified as Ursus abstrusus or Tremarctos floridanus.
† P. cf. harroldorum Taunton
† Pliotaxidea † P. sp. White Bluffs An American badger-like mustelid.
Procyon? P.? sp. Taunton A possible raccoon.
† Satherium † S. piscinarium Taunton An otter.
Spilogale S. sp. Taunton A spotted skunk.
Taxidea T. sp. Taunton An American badger.
† Trigonictis † T. cookii White Bluffs, Taunton An ictonychine (grison-like mustelid). T. cookii may represent small individuals of T. macrodon.

Lagomorpha

Lagomorphs of the Ringold Formation
Genus / Taxon Species Local fauna Notes Images
† Alilepus † A. vagus Taunton A rabbit.
† Hypolagus † H. edensis Taunton A rabbit.
† H. furlongi Taunton
† H. gidleyi Taunton
† H. ringoldensis White Bluffs, Taunton
Leporidae Blufftop An indeterminate rabbit or hare.
† Nekrolagus † N. progressus White Bluffs A rabbit.
† N.? sp. Taunton

Perissodactyla

Perissodactyls of the Ringold Formation
Genus / Taxon Species Local fauna Notes Images
† Aphelops † A. cf. mutilus An aceratheriine rhinoceros, the oldest mammal in the formation.
Equus † Equus francescana White Bluffs A zebra-like horse similar to the Hagerman horse. Sometimes classified as Dolichohippus or Plesippus.
† Equus simplicidens Taunton A zebra-like Hagerman horse. Sometimes classified as Dolichohippus or Plesippus.
Tapirus T. sp. White Bluffs A tapir.
† Teleoceras † T. hicksi River Road, White Bluffs A teleoceratin aceratheriine rhinoceros.

Pilosa

Pilosans of the Ringold Formation
Genus / Taxon Species Local fauna Notes Images
† Megalonyx † M. leptostomus Taunton A megalonychid ground sloth.
† M. rohrmanni White Bluffs A fairly common megalonychid ground sloth.

Proboscidea

Proboscideans of the Ringold Formation
Genus / Taxon Species Local fauna Notes Images
† Mammut † M. americanum White Bluffs The oldest known fossils of the American mastodon.

Rodentia

Rodents of the Ringold Formation
Genus / Taxon Species Local fauna Notes Images
Ammospermophilus † A. hanfordi White Bluffs An antelope squirrel.
Castor † C. californicus White Bluffs, Taunton A beaver.
† Dipoides † D. rexroadensis White Bluffs A very large beaver.
† Mimomys † M. meadensis Taunton A microtine vole. Some fossils of this species were previously known as Ophiomys taylori.
† M. sawrockensis White Bluffs A microtine vole. Some fossils of this species were previously known as Ophiomys mcknighti.
† M. sawrockensis-taylori White Bluffs, Blufftop A microtine vole, intermediate between M. sawrockensis and M. taylori. Some fossils of this population were previously known as Ophiomys mcknighti.
Neotoma (Paraneotoma) † N. (P.) cf. fossilis Taunton A woodrat.
† N. (P.) cf. quadriplicatus White Bluffs
† Paenemarmota † P. sp. White Bluffs A very large marmot.
Perognathus P. sp. Taunton A pocket mouse.
Peromyscus † P. nosher White Bluffs A deer mouse.
Ondatra (Pliopotamys) † O. (P.) minor Taunton A muskrat.
† Procastoroides † P. cf. idahoensis Taunton A beaver.
† Prodipodomys † P. sp. Taunton A heteromyid with similarities to Dipodomys (kangaroo rats).
Spermophilus † S. cf. howelli Taunton A ground squirrel.
† S.? russelli White Bluffs
† S.? cf. russelli Taunton
Thomomys † T. cf. gidleyi White Bluffs, Taunton A smooth-toothed pocket gopher.

Soricomorpha

Soricomorphs of the Ringold Formation
Genus / Taxon Species Local fauna Notes Images
† Paracryptotis † P. rex Blufftop A shrew.
Scapanus S. sp. White Bluffs A broad-footed mole.
Sorex † S. cf. meltoni Taunton A long-tailed shrew.
† S. powersi Blufftop
S. sp. Taunton

Birds

Birds of the Ringold Formation
Genus / Taxon Species Local fauna Notes Images
Aechmophorus A. sp. Taunton A grebe.
Anas A. sp. Taunton A teal-like duck.
Aythya A. sp. Taunton A scaup-like duck.
Branta B. sp. Taunton A black goose.
Dendragapus D. sp. Taunton A grouse.
Fulica F. sp. Taunton A coot.
Podiceps P. sp. Taunton A grebe.

Reptiles

Reptiles of the Ringold Formation
Genus / Taxon Species Local fauna Notes Images
Charina C. bottae Taunton The living rubber boa.
Chelonia White Bluffs, Taunton Indeterminate turtles and tortoises.
Chrysemys? C.? sp. White Bluffs A painted turtle.
Clemmys C. marmorata White Bluffs The living Western pond turtle.
Coluber / Masticophis C. sp. / M. sp. Taunton A racer or whip snake.
Crotalus C. sp. Taunton A rattlesnake.
Elaphe † E. pliocenica Taunton A rat snake.
E. vulpina Taunton The living Eastern foxsnake.
Lampropeltis L. getula Taunton The living common kingsnake.
Pituophis P. catenifer Taunton The living Western gopher snake.
Squamata White Bluffs, Taunton Indeterminate snakes and lizards.
† Tauntonophis † T. morganorum Taunton A colubrine colubrid snake.
Testudo / Geochelone T. sp. / G. sp. White Bluffs A tortoise.
Thamnophis T. sp. Taunton A garter snake.

Amphibians

Indeterminate frog or toad bones are known from the White Bluffs local fauna.

Fish

Fish of the Ringold Formation
Genus / Taxon Species Local fauna Notes Images
Acipenser A. transmontanus White Bluffs, Blufftop, Taunton The living white sturgeon.
Acrocheilus † A. latus Taunton A chiselmouth.
Ameiurus † A. reticulatus White Bluffs, Blufftop, Taunton A bullhead catfish.
Archoplites † A. molarus White Bluffs, Blufftop, Taunton A freshwater sunfish.
Catostomus C. macrocheilus Blufftop, Taunton The living largescale sucker.
Chasmistes † C. sp. cf. batrachops White Bluffs, Blufftop, Taunton A sucker.
Esox † E. columbianus White Bluffs, Blufftop, Taunton A large pike.
† Klamathella † K. milleri Taunton A chub.
Lavinia † L. hibbardi Taunton A hitch.
Mylocheilus † M. heterodon White Bluffs, Blufftop, Taunton A peamouth chub.
Oncorhynchus † O. rastrosus River Road A giant tusked salmon.
Ptychocheilus † P. arciferus Blufftop, Taunton A pikeminnow.

Invertebrates

Several species of freshwater snails are known from the White Bluffs local fauna.

Plants and climate

Pollen has been sampled from the lower Ringold Formation (8.5–5.5 Ma, late Miocene) near Hanford, as well as the upper Ringold Formation (4.5–2.8 Ma) at White Bluffs. The lower Ringold flora is similar to moist eastern ecosystems such as the Mississippi lowland forests, where cypress and broadleaf hardwoods coexist in close proximity. Pollen from White Bluffs corresponds to semi-arid grassland plants such as grasses (Poaceae), saltbush-type plants (Amaranthaceae), and sunflower-type plants (Asteraceae), alongside rare pine pollen.

Warm-water fish and tortoises suggest that the fossil-rich Pliocene portion of the formation probably had hot summers (>27 °C (81 °F)) and mild winters. In warmer parts of the Pliocene, winters may have been entirely frost-free. Pike and sturgeon may indicate the presence of deep, persistent streams (rainfall >80 cm/year (31 in/year)). Other studies estimate a yearly rainfall not exceeding 40 cm/year (16 in/year), still much greater than the modern Columbia Plateau. Riverside floodplain environments were far more common than today, supporting a greater diversity of mammals and wetland inhabitants.

See also

References

  1. 1 2 3 "Paleontology - Hanford Reach". United States Fish and Wildlife Service. Retrieved 2024-11-01.
  2. ↑ David Hagen. "White Bluffs South". Washington Trails Association. Retrieved 2019-12-19.
  3. 1 2 John C. Merriam; John P. Buwalda (1917). Age of strata referred to the Ellensburgh formation in the White Bluffs of the Columbia River. University of California.
  4. 1 2 J. ERIC SCHUSTER; CHARLES W. GULICK; STEPHEN P. REIDEL; KARL R. FECHT; STEPHANIE ZURENKO (1997). "Geologic Map of Washington - Southeast Quadrant" (PDF). Washington State Department of Natural Resources. Retrieved 2019-12-20.
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  6. ↑ Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Archived from the original on 25 March 2022. Retrieved 17 December 2021.
  7. 1 2 R. C. Newcomb (1958). "RINGOLD FORMATION OF PLEISTOCENE AGE IN TYPE LOCALITY, THE WHITE BLUFFS, WASHINGTON" (PDF). Washington State Department of Natural Resources. Retrieved 2019-12-20.
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  10. ↑ Staisch, Lydia M.; O'Connor, Jim E.; Cannon, Charles M.; Holm-Denoma, Chris; Link, Paul K.; Lasher, John; Alexander, Jeremy A. (2021). "Major reorganization of the Snake River modulated by passage of the Yellowstone Hotspot" (PDF). GSA Bulletin. Geological Society of America.
  11. ↑ "Columbia River Basalt Group Stretches from Oregon to Idaho". United States Geological Survey. Archived from the original on 2020-01-13. Retrieved 2019-12-19.
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