Omarolluk
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Omarolluks, sometimes shortened to omars, are a distinctive type of
glacial erratic A glacial erratic is glacially deposited rock differing from the type of rock native to the area in which it rests. Erratics, which take their name from the Latin word ' ("to wander"), are carried by glacial ice, often over distances of hundred ...
that consists of dark siliceous
greywacke Greywacke or graywacke (German ''grauwacke'', signifying a grey, earthy rock) is a variety of sandstone generally characterized by its hardness, dark color, and poorly sorted angular grains of quartz, feldspar, and small rock fragments or lit ...
and exhibits prominent rounded, often deep, hemispherical voids and pits. The hemispherical voids and pits result from the selective dissolution of carbonate
concretion A concretion is a hard, compact mass of matter formed by the precipitation of mineral cement within the spaces between particles, and is found in sedimentary rock or soil. Concretions are often ovoid or spherical in shape, although irregular ...
s within the greywacke. The greywacke is identifiable by its low metamorphic grade and the 10–40% rock fragments, distinctive volcanic clasts, and spherical carbonate concretions that it contains. Omars are typically rounded and range in size from pebbles to boulders. Their rounded shape, whether found in glacial tills or glacial-fluvial (outwash) gravels, indicate that they were eroded from pre-existing
littoral The littoral zone or nearshore is the part of a sea, lake, or river that is close to the shore. In coastal ecology, the littoral zone includes the intertidal zone extending from the high water mark (which is rarely inundated), to coastal areas ...
or
fluvial In geography and geology, fluvial processes are associated with rivers and streams and the deposits and landforms created by them. When the stream or rivers are associated with glaciers, ice sheets, or ice caps, the term glaciofluvial or fluviog ...
deposits. Omars are typically found associated with granules and
pebble A pebble is a clast of rock with a particle size of based on the Udden-Wentworth scale of sedimentology. Pebbles are generally considered larger than granules ( in diameter) and smaller than cobbles ( in diameter). A rock made predominant ...
s of oolitic
jasper Jasper, an aggregate of microgranular quartz and/or cryptocrystalline chalcedony and other mineral phases,Kostov, R. I. 2010. Review on the mineralogical systematics of jasper and related rocks. – Archaeometry Workshop, 7, 3, 209-213PDF/ref> ...
that were transported from the
Belcher Islands The Belcher Islands ( iu, script=latn, ᓴᓪᓚᔪᒐᐃᑦ, Sanikiluaq) are an archipelago in the southeast part of Hudson Bay near the centre of the Nastapoka arc. The Belcher Islands are spread out over almost . Administratively, they belon ...
in
Hudson Bay Hudson Bay ( crj, text=ᐐᓂᐯᒄ, translit=Wînipekw; crl, text=ᐐᓂᐹᒄ, translit=Wînipâkw; iu, text=ᑲᖏᖅᓱᐊᓗᒃ ᐃᓗᐊ, translit=Kangiqsualuk ilua or iu, text=ᑕᓯᐅᔭᕐᔪᐊᖅ, translit=Tasiujarjuaq; french: b ...
,
Canada Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by tot ...
.Donaldson, A. and V.K. Prest (1997) ''Criteria for recognizing omars, widely dispersed indicators of Pleistocene history in North America.'' GAC/MAC Abs. 22:40, Ottawa.Prest, V.K., J.A. Donaldson, and H.D. Mooers (2000) ''The omar story: the role of omars in assessing glacial history of west-central North America.'' Géographie Physique et Quaternaire 54(3):257-270.Mooers, H.D., and J.D. Lehr (1998) ''Terrestrial record of Laurentide Ice Sheet reorganization during Heinrich events: Reply.'' Geology. 26(7):668-669. The name given these glacial erratics refer to their source, which is the
Proterozoic The Proterozoic () is a geological eon spanning the time interval from 2500 to 538.8million years ago. It is the most recent part of the Precambrian "supereon". It is also the longest eon of the Earth's geologic time scale, and it is subdivided ...
Omarolluk Formation in the Belcher Islands in southeast Hudson Bay. The Laurentide Ice Sheet eroded omars from the Belcher Islands, an
archipelago An archipelago ( ), sometimes called an island group or island chain, is a chain, cluster, or collection of islands, or sometimes a sea containing a small number of scattered islands. Examples of archipelagos include: the Indonesian Archi ...
limited to only about a quarter of 1% of Hudson Bay.
Glaciers A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as ...
moved omars from the southeastern part of Hudson Bay to central Canada and into the U.S. where they were deposited on
moraines A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice she ...
. Because scientists know precisely where they came from they are very valuable in documenting the movement of glaciers.Dutch, S. (n.d.
''Leaverites - Features in Sedimentary Rocks.''
Natural and Applied Sciences, University of Wisconsin, Green Bay, Wisconsin Downloaded October 28, 2009
Wilson, G. (2007

Turnstone Geological Services Ltd, Campbellford, Ontario, Canada. Downloaded October 28, 2009


Etymology

There is uncertainty on how to translate the proper name Omarolluk (and omar rocks). According to the records of the Canada Centre for Mapping and Earth Observation Natural Resources, the features Omarolluk Sound and Omarolluk Formation were named after Omarolluk, an Inuit man who accompanied and guided R. J. Flaherty on numerous geological surveys of the
Belcher Islands The Belcher Islands ( iu, script=latn, ᓴᓪᓚᔪᒐᐃᑦ, Sanikiluaq) are an archipelago in the southeast part of Hudson Bay near the centre of the Nastapoka arc. The Belcher Islands are spread out over almost . Administratively, they belon ...
and elsewhere in the Canadian north. He was probably an
Inuktitut Inuktitut (; , syllabics ; from , "person" + , "like", "in the manner of"), also Eastern Canadian Inuktitut, is one of the principal Inuit languages of Canada. It is spoken in all areas north of the tree line, including parts of the provinces o ...
-dialect speaker from the eastern coast of Hudson Bay. The spelling likely varied from the originally pronounced but unrecorded aural form of the name. Despite the expected natural-feature designations, Omarolluk was surely an actual person. There are three possible translations, as follows: (1) Best: In the subdialect ( Itivimiut) of the
Nunavik Nunavik (; ; iu, ᓄᓇᕕᒃ) comprises the northern third of the province of Quebec, part of the Nord-du-Québec region and nearly coterminous with Kativik. Covering a land area of north of the 55th parallel, it is the homeland of the I ...
dialect of
Inuktitut Inuktitut (; , syllabics ; from , "person" + , "like", "in the manner of"), also Eastern Canadian Inuktitut, is one of the principal Inuit languages of Canada. It is spoken in all areas north of the tree line, including parts of the provinces o ...
, the phoneme /j/ was and still is up to a point pronounced more or less like English ''r'' and generally transcribed as such, and so the name in the standard Canadian Inuit spelling might have been *''Uumajurluk'' (pronounced /uumaruRluk/: ''r'' = English ''r''; ''R'' = French ''r''), that is, ‘bad animal’ (''uumajuq'' ‘animal’; ''luk'' ‘bad’) as a guess. (2) Somewhat similar but possibly: ‘poor reason for being alive’, ''uumaq-jjut-luk'' ‘be.alive–reason.for/cause.for–bad/poor’ (-''jjut'' takes the form -''rut'' after the uvular and then deletes it, at least in the contemporary language). The initial ''o'' is dubious for an expected ''u''. (3) A distant
Yup’ik The Yup'ik or Yupiaq (sg & pl) and Yupiit or Yupiat (pl), also Central Alaskan Yup'ik, Central Yup'ik, Alaskan Yup'ik ( own name ''Yup'ik'' sg ''Yupiik'' dual ''Yupiit'' pl; russian: Юпики центральной Аляски), are an I ...
possibility if applied to a rock stratum: ''Umaq'' is a seam between the upper and lower parts of a ''kamik'' (sealskin boot); the ''ruq'' part would mean ‘to become’, and ''luk'' is the ‘it’, thus imperfectly ‘it becomes a seam’, but if ''umaaq'', then it becomes ‘rip (at the seam)’, a verb, which would mean something like ‘it has a habit of ripping at the seam’.Supplied by Carl Masthay, St. Louis, Missouri, 28 January 2019


See also

*
Adder stone An adder stone is a type of stone, usually glassy, with a naturally occurring hole through it. Such stones, which usually consist of flint, have been discovered by archaeologists in both Britain and Egypt. Commonly, they are found in Northern Germ ...
, Eurasian natural rocks with holes. *
Cupstone Cupstones, also called anvil stones, pitted cobbles and nutting stones, among other names, are roughly discoidal or amorphous groundstone artifacts among the most common lithic remains of Native American culture, especially in the Midwestern ...
, true Native American artifacts. *
Pholad borings Pholad borings are tubular burrows in firm clay and soft rock that have been created by bivalve molluscs (boring clams) in the family Pholadidae. The common names of clams in this family are "pholads", "piddocks", and "angel wings"; the latter ...
, similar rock holes caused by certain types of bivalves. *
Lithic technology In archaeology, lithic technology includes a broad array of techniques used to produce usable tools from various types of stone. The earliest stone tools were recovered from modern Ethiopia and were dated to between two-million and three-million ...


References

Prest, V.K. (1990) Laurentide ice-flow patterns: A historical review, and implications of the dispersal of Belcher Island erratics. Géographie Physique et Quaternaire 44(2):113-136. {{Prehistoric technology Sedimentology