Saanich Formation

Last updated
Saanich Formation
Stratigraphic range: Late Pleistocene
Type Formation
Overlies?Sooke formation
Lithology
Primaryunlithified siliciclastic costal marine
Location
Region Puget Sound, Washington (state)
Country United States

The Saanich Formation is a geologic formation in the Puget Sound area of Washington. It consists of Pleistocene marine siloclastic deposits preserving fossils. [1]

See also

Related Research Articles

In linguistics, an affix is a morpheme that is attached to a word stem to form a new word or word form. Affixes may be derivational, like English -ness and pre-, or inflectional, like English plural -s and past tense -ed. They are bound morphemes by definition; prefixes and suffixes may be separable affixes. Affixation is the linguistic process that speakers use to form different words by adding morphemes at the beginning (prefixation), the middle (infixation) or the end (suffixation) of words.

<span class="mw-page-title-main">Mastodon</span> Genus of mammals (fossil)

A mastodon is any proboscidean belonging to the extinct genus Mammut that inhabited North and Central America during the late Miocene or late Pliocene up to their extinction at the end of the Pleistocene 10,000 to 11,000 years ago. Mastodons lived in herds and were predominantly forest-dwelling animals. They generally had a browsing diet, distinct from that of the contemporary Columbian mammoth, which tended towards grazing.

<span class="mw-page-title-main">Saanich, British Columbia</span> Municipality in British Columbia, Canada

Saanich is a district municipality on Vancouver Island in British Columbia, within the Greater Victoria area. The population was 117,735 at the 2021 census, making it the most populous municipality in the Capital Regional District and Vancouver Island, and the eighth-most populous in the province. The district adopted its name after the Saanich First Nation, meaning "emerging land" or "emerging people". The District acts as a bedroom community immediately to the north of Victoria, British Columbia.

<span class="mw-page-title-main">Greater Victoria</span> Metropolitan area in British Columbia, Canada

Greater Victoria is located in British Columbia, Canada, on the southern tip of Vancouver Island. It is usually defined as the thirteen municipalities of the Capital Regional District (CRD) on Vancouver Island as well as some adjacent areas and nearby islands.

<span class="mw-page-title-main">Channeled Scablands</span> Landscape in eastern Washington state scoured by cataclysmic floods during the Pleistocene epoch

The Channeled Scablands are a relatively barren and soil-free region of interconnected relict and dry flood channels, coulees and cataracts eroded into Palouse loess and the typically flat-lying basalt flows that remain after cataclysmic floods within the southeastern part of Washington. The Channeled Scablands were scoured by more than 40 cataclysmic floods during the Last Glacial Maximum and innumerable older cataclysmic floods over the last two million years. These floods were periodically unleashed whenever a large glacial lake broke through its ice dam and swept across eastern Washington and down the Columbia River Plateau during the Pleistocene epoch. The last of the cataclysmic floods occurred between 18,200 and 14,000 years ago.

Saanich is the language of the First Nations Saanich people in the Pacific Northwest region of northwestern North America. Saanich is a Coast Salishan language in the Northern Straits dialect continuum, the varieties of which are closely related to the Klallam language.

Saanich Peninsula is located north of Victoria, British Columbia, Canada. It is bounded by Saanich Inlet on the west, Satellite Channel on the north, the small Colburne Passage on the northeast, and Haro Strait on the east. The exact southern boundary of what is referred to as the "Saanich Peninsula" is somewhat fluid in local parlance.

<span class="mw-page-title-main">Bamberton</span>

Bamberton is an industrial site located on the Saanich Inlet, just south of Mill Bay, around 45k kilometres north of Victoria on Vancouver Island.

<span class="mw-page-title-main">Swan Lake Nature Sanctuary</span> Nature reserve in British Columbia

Swan Lake Christmas Hill Nature Sanctuary is a nature reserve located in Saanich, British Columbia. The sanctuary includes a lake, adjacent marshy lowlands, and the Nature House, as well as a good part of the summit regions of Christmas Hill.

<i>Bison antiquus</i> Extinct species of mammal

Bison antiquus, the antique or ancient bison, is an extinct species of bison that lived in Late Pleistocene North America until around 10,000 years ago. It was one of the most common large herbivores on the North American continent during the late Pleistocene, and is a direct ancestor of the living American bison along with Bison occidentalis.

<i>Platygonus</i>

Platygonus is an extinct genus of herbivorous peccaries of the family Tayassuidae, endemic to North and South America from the Miocene through Pleistocene epochs, existing for about 10.289 million years. P. compressus stood 2.5 feet tall.

<i>Castor californicus</i> Species of mammal (fossil)

Castor californicus is an extinct species of beaver that lived in western North America from the end of the Miocene to the early Pleistocene. The species was similar to but larger than the extant North American beaver, C. canadensis.

Tule Springs Archaeological Site is an archeological site listed on the National Register of Historic Places that is located in the Las Vegas Valley of Nevada, United States. It is one of a few sites in the United States where humans were once thought to have lived alongside, and potentially hunted, extinct Ice Age megafauna, although this view is not supported by the available scientific data and is no longer generally accepted.

<span class="mw-page-title-main">Anastasia Formation</span> Geologic formation deposited in Florida during the Late Pleistocene epoch.

The Anastasia Formation is a geologic formation deposited in Florida during the Late Pleistocene epoch.

Satherium piscinarium is an extinct species of giant otter of North America that lived during the Pliocene through Pleistocene from ~3.7–1.6 Ma. (AEO). existing for approximately 2.1 million years.

<i>Hypolagus</i> Extinct genus of lagomorph

Hypolagus is an extinct genus of lagomorph, first recorded in the Hemingfordian of North America. It entered Asia during the early Turolian and spread to Europe not much later, where it survived until the Middle Pleistocene. Though unknown in the Iberian Peninsula, fossils of this genus have been found in the Balearic Islands, suggesting an eastern migration during the dry period in the Mediterranean region known as the Messinian Salinity Crisis.

<span class="mw-page-title-main">Paleontology in North Carolina</span>

Paleontology in North Carolina refers to paleontological research occurring within or conducted by people from the U. S. state of North Carolina. Fossils are common in North Carolina. According to author Rufus Johnson, "almost every major river and creek east of Interstate 95 has exposures where fossils can be found". The fossil record of North Carolina spans from Eocambrian remains that are 600 million years old, to the Pleistocene 10,000 years ago.

<span class="mw-page-title-main">Paleontology in Maryland</span>

Paleontology in Maryland refers to paleontological research occurring within or conducted by people from the U.S. state of Maryland. The invertebrate fossils of Maryland are similar to those of neighboring Delaware. For most of the early Paleozoic era, Maryland was covered by a shallow sea, although it was above sea level for portions of the Ordovician and Devonian. The ancient marine life of Maryland included brachiopods and bryozoans while horsetails and scale trees grew on land. By the end of the era, the sea had left the state completely. In the early Mesozoic, Pangaea was splitting up. The same geologic forces that divided the supercontinent formed massive lakes. Dinosaur footprints were preserved along their shores. During the Cretaceous, the state was home to dinosaurs. During the early part of the Cenozoic era, the state was alternatingly submerged by sea water or exposed. During the Ice Age, mastodons lived in the state.

<i>Neolicaphrium</i>

Neolicaphrium is an extinct genus of ungulate mammal belonging to the extinct order Litopterna. This animal lived from the Late Pliocene (Chapadmalalan) to the Late Pleistocene (Lujanian) in southern South America, being the last survivor of the family Proterotheriidae.

References

  1. Austin Hendy. "Saanich Fm - Alki Point/Bainbridge Island (Pleistocene of the United States)" . Retrieved 2 August 2022.