Lithostratigraphy, the Glossary
Lithostratigraphy is a sub-discipline of stratigraphy, the geological science associated with the study of strata or rock layers.[1]
Table of Contents
57 relations: Argentina, Biostratigraphy, Canyonlands National Park, Capitol Reef National Park, Chinle Formation, Chronostratigraphy, Coal, Colorado Plateau, Complex (geology), Cutler Formation, Deposition (geology), Diastem, Earth science, Erosion surface, Facies, Fossil, Geochronology, Geological formation, Geology, Glen Canyon National Recreation Area, Igneous rock, Jurassic, Kayenta Formation, Kerogen, Law of superposition, Layered intrusion, Limestone, Lithology, Lithostratigraphy, Magmatism, Metamorphic rock, Moenkopi Formation, Navajo Sandstone, Nicolas Steno, Paleosol, Petrology, Principle of lateral continuity, Principle of original horizontality, Science, Sediment, Sedimentary basin, Sedimentary rock, Sedimentary structures, Shale, Stratigraphic unit, Stratigraphy, Stratotype, Stratum, Strike and dip, Taxonomy (biology), ... Expand index (7 more) »
- Geochronological dating methods
Argentina
Argentina, officially the Argentine Republic, is a country in the southern half of South America.
See Lithostratigraphy and Argentina
Biostratigraphy
Biostratigraphy is the branch of stratigraphy which focuses on correlating and assigning relative ages of rock strata by using the fossil assemblages contained within them. Lithostratigraphy and Biostratigraphy are stratigraphy.
See Lithostratigraphy and Biostratigraphy
Canyonlands National Park
Canyonlands National Park is an American national park located in southeastern Utah near the town of Moab.
See Lithostratigraphy and Canyonlands National Park
Capitol Reef National Park
Capitol Reef National Park is an American national park in south-central Utah.
See Lithostratigraphy and Capitol Reef National Park
Chinle Formation
The Chinle Formation is an Upper Triassic continental geological formation of fluvial, lacustrine, and palustrine to eolian deposits spread across the U.S. states of Nevada, Utah, northern Arizona, western New Mexico, and western Colorado.
See Lithostratigraphy and Chinle Formation
Chronostratigraphy
Chronostratigraphy is the branch of stratigraphy that studies the ages of rock strata in relation to time. Lithostratigraphy and Chronostratigraphy are Geochronological dating methods and stratigraphy.
See Lithostratigraphy and Chronostratigraphy
Coal
Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams.
See Lithostratigraphy and Coal
Colorado Plateau
The Colorado Plateau is a physiographic and desert region of the Intermontane Plateaus, roughly centered on the Four Corners region of the southwestern United States.
See Lithostratigraphy and Colorado Plateau
Complex (geology)
In geology, a complex is a lithodemic unit consisting of two or more lithodemes of more than one genetic class (metamorphic, igneous or sedimentary).
See Lithostratigraphy and Complex (geology)
Cutler Formation
The Cutler Formation or Cutler Group is a rock unit that is exposed across the U.S. states of Arizona, northwest New Mexico, southeast Utah and southwest Colorado.
See Lithostratigraphy and Cutler Formation
Deposition (geology)
Deposition is the geological process in which sediments, soil and rocks are added to a landform or landmass.
See Lithostratigraphy and Deposition (geology)
Diastem
In geology, a diastem is a short interruption in sedimentation with little or no erosion. Lithostratigraphy and diastem are stratigraphy.
See Lithostratigraphy and Diastem
Earth science
Earth science or geoscience includes all fields of natural science related to the planet Earth.
See Lithostratigraphy and Earth science
Erosion surface
In geology and geomorphology, an erosion surface is a surface of rock or regolith that was formed by erosion and not by construction (e.g. lava flows, sediment deposition) nor fault displacement.
See Lithostratigraphy and Erosion surface
Facies
In geology, a facies (same pronunciation and spelling in the plural) is a body of rock with distinctive characteristics. Lithostratigraphy and facies are Petrology and stratigraphy.
See Lithostratigraphy and Facies
Fossil
A fossil (from Classical Latin) is any preserved remains, impression, or trace of any once-living thing from a past geological age.
See Lithostratigraphy and Fossil
Geochronology
Geochronology is the science of determining the age of rocks, fossils, and sediments using signatures inherent in the rocks themselves.
See Lithostratigraphy and Geochronology
Geological formation
A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics (lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exposed in a geographical region (the stratigraphic column).
See Lithostratigraphy and Geological formation
Geology
Geology is a branch of natural science concerned with the Earth and other astronomical objects, the rocks of which they are composed, and the processes by which they change over time.
See Lithostratigraphy and Geology
Glen Canyon National Recreation Area
Glen Canyon National Recreation Area (shortened to Glen Canyon NRA or GCNRA) is a national recreation area and conservation unit of the United States National Park Service that encompasses the area around Lake Powell and lower Cataract Canyon in Utah and Arizona, covering of mostly rugged high desert terrain.
See Lithostratigraphy and Glen Canyon National Recreation Area
Igneous rock
Igneous rock, or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic.
See Lithostratigraphy and Igneous rock
Jurassic
The Jurassic is a geologic period and stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya.
See Lithostratigraphy and Jurassic
Kayenta Formation
The Kayenta Formation is a geological formation in the Glen Canyon Group that is spread across the Colorado Plateau province of the United States, including northern Arizona, northwest Colorado, Nevada, and Utah.
See Lithostratigraphy and Kayenta Formation
Kerogen
Kerogen is solid, insoluble organic matter in sedimentary rocks. Lithostratigraphy and Kerogen are Petrology.
See Lithostratigraphy and Kerogen
Law of superposition
The law of superposition is an axiom that forms one of the bases of the sciences of geology, archaeology, and other fields pertaining to geological stratigraphy. Lithostratigraphy and law of superposition are stratigraphy.
See Lithostratigraphy and Law of superposition
Layered intrusion
A layered intrusion is a large sill-like body of igneous rock which exhibits vertical layering or differences in composition and texture.
See Lithostratigraphy and Layered intrusion
Limestone
Limestone (calcium carbonate) is a type of carbonate sedimentary rock which is the main source of the material lime.
See Lithostratigraphy and Limestone
Lithology
The lithology of a rock unit is a description of its physical characteristics visible at outcrop, in hand or core samples, or with low magnification microscopy. Lithostratigraphy and lithology are Petrology.
See Lithostratigraphy and Lithology
Lithostratigraphy
Lithostratigraphy is a sub-discipline of stratigraphy, the geological science associated with the study of strata or rock layers. Lithostratigraphy and Lithostratigraphy are Geochronological dating methods, Petrology and stratigraphy.
See Lithostratigraphy and Lithostratigraphy
Magmatism
Magmatism is the emplacement of magma within and at the surface of the outer layers of a terrestrial planet, which solidifies as igneous rocks.
See Lithostratigraphy and Magmatism
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism.
See Lithostratigraphy and Metamorphic rock
Moenkopi Formation
The Moenkopi Formation is a geological formation that is spread across the U.S. states of New Mexico, northern Arizona, Nevada, southeastern California, eastern Utah and western Colorado.
See Lithostratigraphy and Moenkopi Formation
Navajo Sandstone
The Navajo Sandstone is a geological formation in the Glen Canyon Group that is spread across the U.S. states of southern Nevada, northern Arizona, northwest Colorado, and Utah as part of the Colorado Plateau province of the United States.
See Lithostratigraphy and Navajo Sandstone
Nicolas Steno
Niels Steensen (Niels Steensen; Latinized to Nicolas Steno or Nicolaus Stenonius); 1 January 1638 – 25 November 1686) was a Danish scientist, a pioneer in both anatomy and geology who became a Catholic bishop in his later years. Steensen was trained in the classical texts on science; however, by 1659 he seriously questioned accepted knowledge of the natural world.
See Lithostratigraphy and Nicolas Steno
Paleosol
In geoscience, paleosol (palaeosol in Great Britain and Australia) is an ancient soil that formed in the past.
See Lithostratigraphy and Paleosol
Petrology
Petrology is the branch of geology that studies rocks, their mineralogy, composition, texture, structure and the conditions under which they form.
See Lithostratigraphy and Petrology
Principle of lateral continuity
The principle of lateral continuity states that layers of sediment initially extend laterally in all directions; in other words, they are laterally continuous. Lithostratigraphy and principle of lateral continuity are stratigraphy.
See Lithostratigraphy and Principle of lateral continuity
Principle of original horizontality
The principle of original horizontality states that layers of sediment are originally deposited horizontally under the action of gravity. Lithostratigraphy and principle of original horizontality are stratigraphy.
See Lithostratigraphy and Principle of original horizontality
Science
Science is a strict systematic discipline that builds and organizes knowledge in the form of testable hypotheses and predictions about the world.
See Lithostratigraphy and Science
Sediment
Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. Lithostratigraphy and Sediment are Petrology.
See Lithostratigraphy and Sediment
Sedimentary basin
Sedimentary basins are region-scale depressions of the Earth's crust where subsidence has occurred and a thick sequence of sediments have accumulated to form a large three-dimensional body of sedimentary rock.
See Lithostratigraphy and Sedimentary basin
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. Lithostratigraphy and Sedimentary rock are Petrology.
See Lithostratigraphy and Sedimentary rock
Sedimentary structures
Sedimentary structures include all kinds of features in sediments and sedimentary rocks, formed at the time of deposition.
See Lithostratigraphy and Sedimentary structures
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2Si2O5(OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.
See Lithostratigraphy and Shale
Stratigraphic unit
A stratigraphic unit is a volume of rock of identifiable origin and relative age range that is defined by the distinctive and dominant, easily mapped and recognizable petrographic, lithologic or paleontologic features (facies) that characterize it. Lithostratigraphy and stratigraphic unit are stratigraphy.
See Lithostratigraphy and Stratigraphic unit
Stratigraphy
Stratigraphy is a branch of geology concerned with the study of rock layers (strata) and layering (stratification). Lithostratigraphy and Stratigraphy are Petrology.
See Lithostratigraphy and Stratigraphy
Stratotype
A stratotype or type section in geology is the physical location or outcrop of a particular reference exposure of a stratigraphic sequence or stratigraphic boundary. Lithostratigraphy and stratotype are stratigraphy.
See Lithostratigraphy and Stratotype
Stratum
In geology and related fields, a stratum (strata) is a layer of rock or sediment characterized by certain lithologic properties or attributes that distinguish it from adjacent layers from which it is separated by visible surfaces known as either bedding surfaces or bedding planes. Lithostratigraphy and stratum are stratigraphy.
See Lithostratigraphy and Stratum
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 Lithostratigraphy and Strike and dip
Taxonomy (biology)
In biology, taxonomy is the scientific study of naming, defining (circumscribing) and classifying groups of biological organisms based on shared characteristics.
See Lithostratigraphy and Taxonomy (biology)
Tephra
Tephra is fragmental material produced by a volcanic eruption regardless of composition, fragment size, or emplacement mechanism.
See Lithostratigraphy and Tephra
Topostratigraphy
Topostratigraphy (topostratigrafi) is a method of establishing stratigraphical units based on a mix of biostratigraphy and lithostratigraphy. Lithostratigraphy and Topostratigraphy are stratigraphy.
See Lithostratigraphy and Topostratigraphy
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. Lithostratigraphy and unconformity are stratigraphy.
See Lithostratigraphy and Unconformity
Utah
Utah is a landlocked state in the Mountain West subregion of the Western United States.
See Lithostratigraphy and Utah
Volcanism
Volcanism, vulcanism, volcanicity, or volcanic activity is the phenomenon where solids, liquids, gases, and their mixtures erupt to the surface of a solid-surface astronomical body such as a planet or a moon.
See Lithostratigraphy and Volcanism
Weathering
Weathering is the deterioration of rocks, soils and minerals (as well as wood and artificial materials) through contact with water, atmospheric gases, sunlight, and biological organisms.
See Lithostratigraphy and Weathering
Wingate Sandstone
The Wingate Sandstone is a geologic formation in the Glen Canyon Group of the Colorado Plateau province of the United States which crops out in northern Arizona, northwest Colorado, Nevada, and Utah.
See Lithostratigraphy and Wingate Sandstone
See also
Geochronological dating methods
- Amino acid dating
- Astrochronology
- Biochronology
- Chronostratigraphy
- Comminution dating
- Detrital zircon geochronology
- Electron spin resonance dating
- Geochronometry
- Incremental dating
- Isotope geochemistry
- Lithostratigraphy
- Luminescence dating
- Monazite geochronology
- Oxygen isotope ratio cycle
- Paleomagnetism
- Radiometric dating
- Reduced chi-squared statistic
- Sensitive high-resolution ion microprobe
- Surface exposure dating
References
[1] https://en.wikipedia.org/wiki/Lithostratigraphy
Also known as Conformably, Lithodeme, Lithodemes, Lithodemic unit, Lithosome, Lithostratigraphic, Lithostratigraphical, Lithostratigraphically.
, Tephra, Topostratigraphy, Unconformity, Utah, Volcanism, Weathering, Wingate Sandstone.