Ringold Formation Explained

Ringold Formation
Type:Formation
Period:Pliocene
Namedfor:Ringold Post Office
Namedby:John C. Merriam, John P. Buwalda
Region:Washington (state)
Country:United States
Coordinates:46.667°N -119.436°W[1]
Underlies:Deposits from Missoula Floods
Overlies:Columbia River Basalt Group
Thickness:1000feet

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 1000feet thick in places.[2] [3] It preserves fossils dating back to the late Miocene and Pliocene epochs of the Neogene period.[4]

Exposures of the Ringold Formation can be found from Hanford Reach National Monument north to the Moses Lake area.[5] 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.[6] [7]

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.[8]

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 4feet thick.[9]

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.[10] 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

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.[11] 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.[12]

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.[13]

Paleobiota

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 / TaxonSpeciesLocal faunaNotesImages
AntilocapridaeWhite BluffsIndeterminate pronghorns.
† Bretzia[19] † B. pseudalcesWhite BluffsA very common capreoline deer with palmate antlers similar to moose. One of the earliest deer in North America.[20]
† Camelops† C. sp.Taunton[21] A large camel.
† Capromeryx† C. tauntonensisTauntonAn antilocaprid (pronghorn). Later Capromeryx species were quite small, but this early species was only slightly smaller than living pronghorns.
CervidaeBlufftop, TauntonIndeterminate deer. Some Taunton fossils are similar to Odocoileus (mule deer and kin) and Rangifer (reindeer).
† Hemiauchenia† H. blancoensisWhite Bluffs,[22] TauntonA common lamine camelid (related to llamas, alpacas, and kin).
† Megatylopus† M. sp. aff. M. gigasRiver Road,White BluffsA common large camel, either M. gigas or M. cochrani.
† Platygonus† P. pearceiWhite BluffsA common flat-headed peccary.
† P. sp.Taunton

Carnivora

Carnivorans of the Ringold Formation
Genus / TaxonSpeciesLocal faunaNotesImages
BassariscusB. astutusWhite Bluffs, TauntonThe living ringtail, a species of procyonid (raccoon-like mammals).
† Borophagus† B. diversidensTaunton[23] A very large borophagine (bone-crushing dog).
† B. hilliWhite Bluffs
† Buisnictis† B. cf. breviramusTauntonA skunk.
Canis† C. lepophagusTauntonA coyote-like canine.
† Chasmaporthetes† C. ossifragusWhite BluffsA long-limbed hyena.
† Dinofeliscf. † D. paleooncaTauntonA possible machairodontine (saber-toothed cat).
† Eucyon† E. davisiWhite BluffsA coyote-like canine, previously classified as a species of Canis.
"Felis"F. sp.White Bluffs, TauntonA cougar-sized cat, probably the same as Puma lacustris or "Lynx rexroadensis".
cf. † Homotheriumcf. † H. sp.White BluffsA relatively small machairodontine (saber-toothed cat).
† Huracan[24] † H. cf. schneideriWhite Bluffs[25] A large ailuropodine (panda-like) bear, previously considered a species of Agriotherium. One of the last surviving ailuropodine bears in North America.
LynxL. cf. rufusTauntonA possible bobcat.
Mustela† M. cf. rexroadensisTauntonA weasel.
† Parailurus† P. sp.Taunton[26] A large ailurid (red panda-like mammal).
† Plionarctos† P. harroldorum[27] White BluffsA 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. harroldorumTaunton
† Pliotaxidea† P. sp.White BluffsAn American badger-like mustelid.
Procyon?P.? sp.TauntonA possible raccoon.
† Satherium† S. piscinariumTauntonAn otter.
SpilogaleS. sp.TauntonA spotted skunk.
TaxideaT. sp.TauntonAn American badger.
† Trigonictis† T. cookiiWhite Bluffs, TauntonAn ictonychine (grison-like mustelid). T. cookii may represent small individuals of T. macrodon.

Lagomorpha

Lagomorphs of the Ringold Formation
Genus / TaxonSpeciesLocal faunaNotesImages
† Alilepus† A. vagusTaunton[28] A rabbit.
† Hypolagus† H. edensisTauntonA rabbit.
† H. furlongiTaunton
† H. gidleyiTaunton
† H. ringoldensisWhite Bluffs, Taunton
LeporidaeBlufftopAn indeterminate rabbit or hare.
† Nekrolagus† N. progressusWhite BluffsA rabbit.
† N.? sp.Taunton

Perissodactyla

Perissodactyls of the Ringold Formation
Genus / TaxonSpeciesLocal faunaNotesImages
† Aphelops† A. cf. mutilusAn aceratheriine rhinoceros, the oldest mammal in the formation.[29]
Equus† Equus francescanaWhite BluffsA zebra-like horse similar to the Hagerman horse. Sometimes classified as Dolichohippus or Plesippus.
† Equus simplicidensTauntonA zebra-like Hagerman horse. Sometimes classified as Dolichohippus or Plesippus.
TapirusT. sp.White BluffsA tapir.
† Teleoceras† T. hicksiRiver Road,[30] White BluffsA teleoceratin aceratheriine rhinoceros.

Pilosa

Pilosans of the Ringold Formation
Genus / TaxonSpeciesLocal faunaNotesImages
† Megalonyx† M. leptostomusTauntonA megalonychid ground sloth.
† M. rohrmanniWhite BluffsA fairly common megalonychid ground sloth.

Rodentia

Rodents of the Ringold Formation
Genus / TaxonSpeciesLocal faunaNotesImages
Ammospermophilus† A. hanfordiWhite BluffsAn antelope squirrel.
Castor† C. californicusWhite Bluffs, TauntonA beaver.
† Dipoides† D. rexroadensisWhite BluffsA very large beaver.
† Mimomys† M. meadensisTaunton[31] A microtine vole. Some fossils of this species were previously known as Ophiomys taylori.
† M. sawrockensisWhite BluffsA microtine vole. Some fossils of this species were previously known as Ophiomys mcknighti.
† M. sawrockensis-tayloriWhite Bluffs, BlufftopA 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. fossilisTauntonA woodrat.
† N. (P.) cf. quadriplicatusWhite Bluffs
† Paenemarmota† P. sp.White BluffsA very large marmot.
PerognathusP. sp.TauntonA pocket mouse.
Peromyscus† P. nosherWhite BluffsA deer mouse.
Ondatra (Pliopotamys)† O. (P.) minorTauntonA muskrat.
† Procastoroides† P. cf. idahoensisTauntonA beaver.
† Prodipodomys† P. sp.TauntonA heteromyid with similarities to Dipodomys (kangaroo rats).
Spermophilus† S. cf. howelliTauntonA ground squirrel.
† S.? russelliWhite Bluffs
† S.? cf. russelliTaunton
Thomomys† T. cf. gidleyiWhite Bluffs, TauntonA smooth-toothed pocket gopher.

Soricomorpha

Soricomorphs of the Ringold Formation
Genus / TaxonSpeciesLocal faunaNotesImages
† Paracryptotis† P. rexBlufftopA shrew.
ScapanusS. sp.White BluffsA broad-footed mole.
Sorex† S. cf. meltoniTauntonA long-tailed shrew.
† S. powersiBlufftop
S. sp.Taunton

Birds

Birds of the Ringold Formation
Genus / TaxonSpeciesLocal faunaNotesImages
AechmophorusA. sp.TauntonA grebe.
AnasA. sp.TauntonA teal-like duck.
AythyaA. sp.TauntonA scaup-like duck.
BrantaB. sp.TauntonA black goose.
DendragapusD. sp.TauntonA grouse.
FulicaF. sp.TauntonA coot.
PodicepsP. sp.TauntonA grebe.

Reptiles

Reptiles of the Ringold Formation
Genus / TaxonSpeciesLocal faunaNotesImages
CharinaC. bottaeTauntonThe living rubber boa.
CheloniaWhite Bluffs, TauntonIndeterminate turtles and tortoises.
Chrysemys?C.? sp.White BluffsA painted turtle.
ClemmysC. marmorataWhite BluffsThe living Western pond turtle.
Coluber / MasticophisC. sp. / M. sp.TauntonA racer or whip snake.
CrotalusC. sp.TauntonA rattlesnake.
Elaphe† E. pliocenicaTauntonA rat snake.
E. vulpinaTauntonThe living Eastern foxsnake.
LampropeltisL. getulaTauntonThe living common kingsnake.
PituophisP. cateniferTauntonThe living Western gopher snake.
SquamataWhite Bluffs, TauntonIndeterminate snakes and lizards.
† Tauntonophis† T. morganorumTauntonA colubrine colubrid snake.
Testudo / GeocheloneT. sp. / G. sp.White BluffsA tortoise.
ThamnophisT. sp.TauntonA garter snake.

Amphibians

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

Fish

Fish of the Ringold Formation
Genus / TaxonSpeciesLocal faunaNotesImages
AcipenserA. transmontanusWhite Bluffs, Blufftop, Taunton[32] The living white sturgeon.
Acrocheilus† A. latusTauntonA chiselmouth.
Ameiurus† A. reticulatusWhite Bluffs, Blufftop, TauntonA bullhead catfish.
Archoplites† A. molarusWhite Bluffs, Blufftop, TauntonA freshwater sunfish.
CatostomusC. macrocheilusBlufftop, TauntonThe living largescale sucker.
Chasmistes† C. sp. cf. batrachopsWhite Bluffs, Blufftop, TauntonA sucker.
Esox† E. columbianusWhite Bluffs, Blufftop, TauntonA large pike.
† Klamathella† K. milleriTauntonA chub.
Lavinia† L. hibbardiTauntonA hitch.
Mylocheilus† M. heterodonWhite Bluffs, Blufftop, TauntonA peamouth chub.
Oncorhynchus† O. rastrosusRiver RoadA giant tusked salmon.
Ptychocheilus† P. arciferusBlufftop, TauntonA 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.[33]

Warm-water fish and tortoises suggest that the fossil-rich Pliocene portion of the formation probably had hot summers (>27C) 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 >80cm/yr). Other studies estimate a yearly rainfall not exceeding 40cm/yr, 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

Notes and References

  1. Web site: White Bluffs South . David Hagen . Washington Trails Association . 2019-12-19.
  2. Web site: Columbia River . . 2019-12-19.
  3. Web site: Paleontology - Hanford Reach. . 2024-11-01.
  4. Web site: Fossilworks: Gateway to the Paleobiology Database. ((Various Contributors to the Paleobiology Database)). 17 December 2021. 25 March 2022. https://web.archive.org/web/20220325060448/http://www.fossilworks.org/cgi-bin/bridge.pl?action=home. dead.
  5. Web site: Geologic Map of Washington - Southeast Quadrant . J. ERIC SCHUSTER . CHARLES W. GULICK . STEPHEN P. REIDEL . KARL R. FECHT . STEPHANIE ZURENKO . Washington State Department of Natural Resources . 1997 . 2019-12-20.
  6. Book: Age of strata referred to the Ellensburgh formation in the White Bluffs of the Columbia River . John C. Merriam . John P. Buwalda . University of California . 1917.
  7. Hanford Quadrangle . C.P. McKinley . 1:62,500 . . 1922 . 2019-12-20.
  8. 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 . GSA Bulletin . Geological Society of America.
  9. Web site: RINGOLD FORMATION OF PLEISTOCENE AGE IN TYPE LOCALITY, THE WHITE BLUFFS, WASHINGTON . R. C. Newcomb . Washington State Department of Natural Resources . 1958 . 2019-12-20.
  10. Web site: Columbia River Basalt Group Stretches from Oregon to Idaho . . 2019-12-19 . 2020-01-13 . https://web.archive.org/web/20200113182530/https://volcanoes.usgs.gov/observatories/cvo/cvo_columbia_river_basalt.html . dead .
  11. Web site: A Geological Paradise . https://web.archive.org/web/20191220053833/https://www.visitthereach.org/a-geological-paradise/ . usurped . December 20, 2019 . . 2019-12-19.
  12. Web site: Past, Present, Future Erosion at Locke Island . B. N. Bjornstad . . 2006 . 2019-12-20.
  13. Web site: Hydrogeologic Controls and Impacts of Quaternary Landslides Along the White Bluffs of the Columbia River, South-Central Washington . Bruce N. Bjornstad . Robert E. Peterson . . 2019-12-20.
  14. Book: Bell . Christopher J. . 7. The Blancan, Irvingtonian, and Rancholabrean Mammal Ages . 2004-04-21 . Late Cretaceous and Cenozoic Mammals of North America: Biostratigraphy and Geochronology . 232–314 . Woodburne . Michael O. . https://www.researchgate.net/publication/263425514 . Columbia University Press . en . 10.7312/wood13040-009 . 978-0-231-50378-5 . Lundelius . Ernest L. . Barnosky . Anthony D. . Graham . Russell W. . Lindsay . Everett H. . Ruez . Dennis R. . Semken . Holmes A. . Webb . S. David . Zakrzewski . Richard J. .
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  16. Gustafson . Eric Paul . May 2015 . Bassariscus from the Early Pliocene of Washington . Northwest Science . 89 . 2 . 129–135 . 10.3955/046.089.0204 . 0029-344X .
  17. Gustafson . Eric Paul . 2015 . An early Pliocene North American deer: Bretzia pseudalces, its osteology, biology, and place in cervid history . Bulletin of the Museum of Natural and Cultural History, University of Oregon . 25.
  18. Gustafson . Eric Paul . 1985 . Soricids (Mammalia, Insectivora) from the Blufftop Local Fauna, Blancan Ringold Formation of Central Washington, and the correlation of Ringold Formation faunas . Journal of Vertebrate Paleontology . 5 . 1 . 88–92 . 10.1080/02724634.1985.10011846 . 0272-4634.
  19. Fry . Willis E. . Gustafson . Eric Paul . 1974 . Cervids from the Pliocene and Pleistocene of Central Washington . Journal of Paleontology . 48 . 2 . 375–386 . 1303258.
  20. Gustafson . Eric Paul . 1985 . Antlers of Bretzia and Odocoileus (Mammalia, Cervidae) and the Evolution of New World Deer . Transactions of the Nebraska Academy of Sciences . 8 . 83-92.
  21. Morgan . James K. . Morgan . Neil H. . 1995-03-14 . A New Species of Capromeryx (Mammalia: Artiodactyla) From the Taunton Local Fauna of Washington, and the Correlation with Other Blancan Faunas of Washington and Idaho . Journal of Vertebrate Paleontology . 15 . 1 . 160–170 . 10.1080/02724634.1995.10011215 . 0272-4634 . 4523614. subscription .
  22. Gustafson . Eric Paul . 1978 . The Vertebrate Faunas of the Pliocene Ringold Formation, South-Central Washington . Bulletin of the Museum of Natural History, University of Oregon . 23.
  23. Wang . Xiaoming . Tedford . Richard R. . Taylor . Beryl E. . 1999 . Phylogenetic Systematics of the Borophaginae (Carnivora: Canidae) . Bulletin of the American Museum of Natural History . 243.
  24. Jiangzuo . Qigao . Flynn . John J. . Wang . Shiqi . Hou . Sukuan . Deng . Tao . 2023-03-14 . New Fossil Giant Panda Relatives (Ailuropodinae, Ursidae): A Basal Lineage of Gigantic Mio-Pliocene Cursorial Carnivores . American Museum Novitates . 2023 . 3996 . 10.1206/3996.1 . 0003-0082.
  25. Martin . James E. . 2013 . A late occurrence of the bear Agriotherium from the Blancan ringold formation in southeastern Washington . Proceedings of the South Dakota Academy of Science . 92 . 123–126.
  26. Tedford . R. H. . Gustafson . E. P. . 1977 . First North American record of the extinct panda Parailurus . Nature . en . 265 . 5595 . 621–623 . 10.1038/265621a0 . 1476-4687. subscription .
  27. Tedford . Richard H. . and Martin . James . 2001-07-20 . Plionarctos, a tremarctine bear (Ursidae: Carnivora) from western North America . Journal of Vertebrate Paleontology . 21 . 2 . 311–321 . 10.1671/0272-4634(2001)021[0311:PATBUC]2.0.CO;2 . 0272-4634 . 20061955.
  28. White . John A. . Morgan . Neil H. . 1995-06-13 . The Leporidae (Mammalia, Lagomorpha) from the Blancan (Pliocene) Taunton Local Fauna of Washington . Journal of Vertebrate Paleontology . 15 . 2 . 366–374 . 10.1080/02724634.1995.10011235 . 0272-4634 . 4523636. subscription .
  29. Gustafson . Eric P. . 2012 . New records of rhinoceroses from the Ringold Formation of central Washington and the Hemphillian-Blancan boundary . Journal of Vertebrate Paleontology . en . 32 . 3 . 727–731 . 10.1080/02724634.2012.658481 . 0272-4634.
  30. Gustafson . Eric Paul . 1977 . First record of Teleoceras (Rhinocerotidae) from the Ringold Formation, Pliocene of Washington . PaleoBios . 27 . 1-4.
  31. Repenning . Charles A. . 2003 . Chapter 17: Mimomys in North America . Bulletin of the American Museum of Natural History . en . 279 . 469–512 . 10.1206/0003-0090(2003)279<0469:C>2.0.CO;2 . 0003-0090. subscription .
  32. Smith . Gerald R. . Morgan . Neil . Gustafson . Eric . 2000 . Fishes of the Mio-Pliocene Ringold Formation, Washington: Pliocene Capture of the Snake River by the Columbia River. . University of Michigan Papers on Paleontology . 32.
  33. Mustoe . George E. . Leopold . Estella B. . 2014 . Paleobotanical evidence for the post-Miocene uplift of the Cascade Range . Canadian Journal of Earth Sciences . 51 . 8 . 809–824 . 10.1139/cjes-2013-0223 . 0008-4077.