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Nastapoka arc, the Glossary

Index Nastapoka arc

The Nastapoka arc is a curved segment of the southeastern shore of Hudson Bay in Quebec, Canada, that extends from the most northerly of the Hopewell Islands to Long Island near the junction with James Bay.[1]

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Table of Contents

  1. 72 relations: Archean, Banded iron formation, Basalt, Bedrock, Belcher Islands, Breccia, Canada, Canoe, Clearwater Lakes, Coast, Conglomerate (geology), Dolomite (rock), Earth, Earth science, Fault (geology), Feldspar, First Nations in Canada, Fluvial sediment processes, Fold (geology), Fold and thrust belt, Foliation (geology), Geologist, Gneiss, Graben, Granite, Granitoid, Granodiorite, Greenschist, Greenstone belt, Homocline, Hudson Bay, Igneous intrusion, Impact crater, Impact structure, Intrusive rock, Inuit, James Bay, Landscape, Lava, List of possible impact structures on Earth, Lithospheric flexure, Long Island (Hudson Bay, Nunavut), Mare Crisium, Mars, Metamorphic rock, Migmatite, Moon, Mudstone, Mylonite, Ottawa Islands, ... Expand index (22 more) »

  2. Geology of Quebec
  3. Hudson Bay

Archean

The Archean Eon (also spelled Archaean or Archæan), in older sources sometimes called the Archaeozoic, is the second of the four geologic eons of Earth's history, preceded by the Hadean Eon and followed by the Proterozoic.

See Nastapoka arc and Archean

Banded iron formation

Banded iron formations (BIFs; also called banded ironstone formations) are distinctive units of sedimentary rock consisting of alternating layers of iron oxides and iron-poor chert.

See Nastapoka arc and Banded iron formation

Basalt

Basalt is an aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the surface of a rocky planet or moon.

See Nastapoka arc and Basalt

Bedrock

In geology, bedrock is solid rock that lies under loose material (regolith) within the crust of Earth or another terrestrial planet.

See Nastapoka arc and Bedrock

Belcher Islands

The Belcher Islands (ᓴᓪᓚᔪᒐᐃᑦ, Sanikiluaq) are an archipelago in the southeast part of Hudson Bay near the centre of the Nastapoka arc.

See Nastapoka arc and Belcher Islands

Breccia

Breccia is a rock composed of large angular broken fragments of minerals or rocks cemented together by a fine-grained matrix.

See Nastapoka arc and Breccia

Canada

Canada is a country in North America.

See Nastapoka arc and Canada

Canoe

A canoe is a lightweight narrow water vessel, typically pointed at both ends and open on top, propelled by one or more seated or kneeling paddlers facing the direction of travel and using paddles.

See Nastapoka arc and Canoe

Clearwater Lakes

The Lac Wiyâshâkimî (the official name, in French, formerly Lac à l'Eau Claire, a calque of the lake's name, Wiyâšâkamî, in Northern East Cree, changed form of wâšâkamî or wâšekamî in more southerly Cree dialects), also called the Clearwater Lakes in English and Allait Qasigialingat by the Inuit, are a pair of annular lakes and impact structures on the Canadian Shield in Quebec, Canada, near Hudson Bay.

See Nastapoka arc and Clearwater Lakes

Coast

A coastalso called the coastline, shoreline, or seashoreis the land next to the sea or the line that forms the boundary between the land and the ocean or a lake.

See Nastapoka arc and Coast

Conglomerate (geology)

Conglomerate is a clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts.

See Nastapoka arc and Conglomerate (geology)

Dolomite (rock)

Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2.

See Nastapoka arc and Dolomite (rock)

Earth

Earth is the third planet from the Sun and the only astronomical object known to harbor life.

See Nastapoka arc and Earth

Earth science

Earth science or geoscience includes all fields of natural science related to the planet Earth.

See Nastapoka arc and Earth science

Fault (geology)

In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements.

See Nastapoka arc and Fault (geology)

Feldspar

Feldspar (sometimes spelled felspar) is a group of rock-forming aluminium tectosilicate minerals, also containing other cations such as sodium, calcium, potassium, or barium.

See Nastapoka arc and Feldspar

First Nations in Canada

First Nations (Premières Nations) is a term used to identify Indigenous peoples in Canada who are neither Inuit nor Métis.

See Nastapoka arc and First Nations in Canada

Fluvial sediment processes

In geography and geology, fluvial sediment processes or fluvial sediment transport are associated with rivers and streams and the deposits and landforms created by sediments.

See Nastapoka arc and Fluvial sediment processes

Fold (geology)

In structural geology, a fold is a stack of originally planar surfaces, such as sedimentary strata, that are bent or curved ("folded") during permanent deformation.

See Nastapoka arc and Fold (geology)

Fold and thrust belt

A fold and thrust belt (FTB) is a series of mountainous foothills adjacent to an orogenic belt, which forms due to contractional tectonics.

See Nastapoka arc and Fold and thrust belt

Foliation (geology)

Foliation in geology refers to repetitive layering in metamorphic rocks.

See Nastapoka arc and Foliation (geology)

Geologist

A geologist is a scientist who studies the structure, composition, and history of Earth.

See Nastapoka arc and Geologist

Gneiss

Gneiss is a common and widely distributed type of metamorphic rock.

See Nastapoka arc and Gneiss

Graben

In geology, a graben is a depressed block of the crust of a planet or moon, bordered by parallel normal faults.

See Nastapoka arc and Graben

Granite

Granite is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase.

See Nastapoka arc and Granite

Granitoid

A granitoid is a generic term for a diverse category of coarse-grained igneous rocks that consist predominantly of quartz, plagioclase, and alkali feldspar.

See Nastapoka arc and Granitoid

Granodiorite

Granodiorite is a coarse-grained (phaneritic) intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar.

See Nastapoka arc and Granodiorite

Greenschist

Greenschists are metamorphic rocks that formed under the lowest temperatures and pressures usually produced by regional metamorphism, typically and 2–10 kilobars.

See Nastapoka arc and Greenschist

Greenstone belt

Greenstone belts are zones of variably metamorphosed mafic to ultramafic volcanic sequences with associated sedimentary rocks that occur within Archaean and Proterozoic cratons between granite and gneiss bodies.

See Nastapoka arc and Greenstone belt

Homocline

In structural geology, a homocline or homoclinal structure (from old homo.

See Nastapoka arc and Homocline

Hudson Bay

Hudson Bay, sometimes called Hudson's Bay (usually historically), is a large body of saltwater in northeastern Canada with a surface area of.

See Nastapoka arc and Hudson Bay

Igneous intrusion

In geology, an igneous intrusion (or intrusive body or simply intrusion) is a body of intrusive igneous rock that forms by crystallization of magma slowly cooling below the surface of the Earth.

See Nastapoka arc and Igneous intrusion

Impact crater

An impact crater is a depression in the surface of a solid astronomical body formed by the hypervelocity impact of a smaller object.

See Nastapoka arc and Impact crater

Impact structure

An impact structure is a generally circular or craterlike geologic structure of deformed bedrock or sediment produced by impact on a planetary surface, whatever the stage of erosion of the structure.

See Nastapoka arc and Impact structure

Intrusive rock

Intrusive rock is formed when magma penetrates existing rock, crystallizes, and solidifies underground to form intrusions, such as batholiths, dikes, sills, laccoliths, and volcanic necks.

See Nastapoka arc and Intrusive rock

Inuit

Inuit (ᐃᓄᐃᑦ 'the people', singular: Inuk, ᐃᓄᒃ, dual: Inuuk, ᐃᓅᒃ; Iñupiaq: Iñuit 'the people'; Greenlandic: Inuit) are a group of culturally and historically similar Indigenous peoples traditionally inhabiting the Arctic and subarctic regions of North America, including Greenland, Labrador, Quebec, Nunavut, the Northwest Territories, Yukon (traditionally), Alaska, and Chukotsky District of Chukotka Autonomous Okrug, Russia.

See Nastapoka arc and Inuit

James Bay

James Bay (Baie James; dirty water) is a large body of water located on the southern end of Hudson Bay in Canada.

See Nastapoka arc and James Bay

Landscape

A landscape is the visible features of an area of land, its landforms, and how they integrate with natural or human-made features, often considered in terms of their aesthetic appeal.

See Nastapoka arc and Landscape

Lava

Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface.

See Nastapoka arc and Lava

List of possible impact structures on Earth

According to the Planetary and Space Science Centre (PASSC) at the University of New Brunswick in Canada, there are 190 confirmed impact structures on Earth.

See Nastapoka arc and List of possible impact structures on Earth

Lithospheric flexure

In geology, lithospheric flexure (also called regional isostasy) is the process by which the lithosphere (rigid, thin outer layer of the Earth) bends under the action of forces such as the weight of a growing orogeny or changes in ice thickness related to glaciation.

See Nastapoka arc and Lithospheric flexure

Long Island (Hudson Bay, Nunavut)

Long Island is one of the many uninhabited Canadian arctic islands in Qikiqtaaluk Region, Nunavut.

See Nastapoka arc and Long Island (Hudson Bay, Nunavut)

Mare Crisium

Mare Crisium (Latin crisium, the "Sea of Crises") is a lunar mare located in the Moon's Crisium basin, just northeast of Mare Tranquillitatis.

See Nastapoka arc and Mare Crisium

Mars

Mars is the fourth planet from the Sun.

See Nastapoka arc and Mars

Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism.

See Nastapoka arc and Metamorphic rock

Migmatite

Migmatite is a composite rock found in medium and high-grade metamorphic environments, commonly within Precambrian cratonic blocks.

See Nastapoka arc and Migmatite

Moon

The Moon is Earth's only natural satellite.

See Nastapoka arc and Moon

Mudstone

Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds.

See Nastapoka arc and Mudstone

Mylonite

Mylonite is a fine-grained, compact metamorphic rock produced by dynamic recrystallization of the constituent minerals resulting in a reduction of the grain size of the rock.

See Nastapoka arc and Mylonite

Ottawa Islands

The Ottawa Islands (Inuit: Arviliit or Arqvilliit in Inuktitut meaning "place where you see bowhead whales") are a group of currently uninhabited islands situated in the eastern edge of Canada's Hudson Bay.

See Nastapoka arc and Ottawa Islands

Pillow lava

Pillow lavas are lavas that contain characteristic pillow-shaped structures that are attributed to the extrusion of the lava underwater, or subaqueous extrusion.

See Nastapoka arc and Pillow lava

Planetary geology

Planetary geology, alternatively known as astrogeology or exogeology, is a planetary science discipline concerned with the geology of celestial bodies such as planets and their moons, asteroids, comets, and meteorites.

See Nastapoka arc and Planetary geology

Proterozoic

The Proterozoic is the third of the four geologic eons of Earth's history, spanning the time interval from 2500 to 538.8Mya, the longest eon of the Earth's geologic time scale.

See Nastapoka arc and Proterozoic

Pseudotachylyte

Pseudotachylyte (sometimes written as pseudotachylite) is an extremely fine-grained to glassy, dark, cohesive rock occurring as veinsTrouw, R.A.J., C.W. Passchier, and D.J. Wiersma (2010) Atlas of Mylonites- and related microstructures. Springer-Verlag, Berlin, Germany.

See Nastapoka arc and Pseudotachylyte

Quartz diorite

Quartz diorite is an igneous, plutonic (intrusive) rock, of felsic composition, with phaneritic texture.

See Nastapoka arc and Quartz diorite

Quartz monzonite

Quartz monzonite is an intrusive, felsic, igneous rock that has an approximately equal proportion of orthoclase and plagioclase feldspars.

See Nastapoka arc and Quartz monzonite

Quebec

QuebecAccording to the Canadian government, Québec (with the acute accent) is the official name in Canadian French and Quebec (without the accent) is the province's official name in Canadian English is one of the thirteen provinces and territories of Canada.

See Nastapoka arc and Quebec

Robert S. Dietz

Robert Sinclair Dietz (September 14, 1914 – May 19, 1995) was a scientist with the United States Coast and Geodetic Survey.

See Nastapoka arc and Robert S. Dietz

Sandstone

Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains, cemented together by another mineral.

See Nastapoka arc and Sandstone

Sedimentary rock

Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation.

See Nastapoka arc and Sedimentary rock

Sedimentary structures

Sedimentary structures include all kinds of features in sediments and sedimentary rocks, formed at the time of deposition.

See Nastapoka arc and Sedimentary structures

Shatter cone

Shatter cones are rare geological features that are only known to form in the bedrock beneath meteorite impact craters or underground nuclear explosions.

See Nastapoka arc and Shatter cone

Strike and dip

In geology, strike and dip is a measurement convention used to describe the plane orientation or attitude of a planar geologic feature.

See Nastapoka arc and Strike and dip

Stromatolite

Stromatolites or stromatoliths are layered sedimentary formations (microbialite) that are created mainly by photosynthetic microorganisms such as cyanobacteria, sulfate-reducing bacteria, and Pseudomonadota (formerly proteobacteria).

See Nastapoka arc and Stromatolite

Structural basin

A structural basin is a large-scale structural formation of rock strata formed by tectonic warping (folding) of previously flat-lying strata into a syncline fold.

See Nastapoka arc and Structural basin

Suevite

Suevite is a rock consisting partly of melted material, typically forming a breccia containing glass and crystal or lithic fragments, formed during an impact event.

See Nastapoka arc and Suevite

Superior Craton

The Superior Craton is a stable crustal block covering Quebec, Ontario, and southeast Manitoba in Canada, and northern Minnesota in the United States. Nastapoka arc and Superior Craton are geology of Quebec.

See Nastapoka arc and Superior Craton

Trans-Hudson orogeny

The Trans-Hudson orogeny or Trans-Hudsonian orogeny was the major mountain building event (orogeny) that formed the Precambrian Canadian Shield and the North American Craton (also called Laurentia), forging the initial North American continent.

See Nastapoka arc and Trans-Hudson orogeny

Turbidite

A turbidite is the geologic deposit of a turbidity current, which is a type of amalgamation of fluidal and sediment gravity flow responsible for distributing vast amounts of clastic sediment into the deep ocean.

See Nastapoka arc and Turbidite

Types of volcanic eruptions

Several types of volcanic eruptions—during which material is expelled from a volcanic vent or fissure—have been distinguished by volcanologists.

See Nastapoka arc and Types of volcanic eruptions

Unconformity

An unconformity is a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous.

See Nastapoka arc and Unconformity

Volcanic rock

Volcanic rocks (often shortened to volcanics in scientific contexts) are rocks formed from lava erupted from a volcano.

See Nastapoka arc and Volcanic rock

See also

Geology of Quebec

Hudson Bay

References

[1] https://en.wikipedia.org/wiki/Nastapoka_arc

, Pillow lava, Planetary geology, Proterozoic, Pseudotachylyte, Quartz diorite, Quartz monzonite, Quebec, Robert S. Dietz, Sandstone, Sedimentary rock, Sedimentary structures, Shatter cone, Strike and dip, Stromatolite, Structural basin, Suevite, Superior Craton, Trans-Hudson orogeny, Turbidite, Types of volcanic eruptions, Unconformity, Volcanic rock.