clastic. shale. clastic. fossiliferous limestone. crystalline, fizzes with acid. Study with Quizlet and memorize flashcards containing terms like sandstone, gypsum, dolostone and more.Crystalline, Clastic, Bioclastic, Oolitic, Etc. Composition of Major Fraction: Composition as Indicated in left column (prefix appropriate names for mixtures) Chiefly Calcite or Dolomite: Composition of Minor Fraction < 10% Minor Fraction : Limestone, Dolomite, Etc.: All varieties in the Calcite-Dolomite horizontal column are possibe here.They consist of 50 percent or more calcite and aragonite (both CaCO3). Dolomites are mainly produced by the secondary alteration or replacement of limestones; i.e., the mineral dolomite [CaMg (CO3)2] replaces the calcite and aragonite minerals in limestones during diagenesis.If non-clastic rocks are fine-grained enough, they too can be called aphanitic. Clastic sedimentary rocks are subdivided on the basis of grain size. Secondary characteristics used to further distinguish clastic rocks are sorting, grain shape, and grain composition. Grain size: Clastic sediments are distinguished on the basis of average grain size. Clastic or detrital sedimentary rocks are made from pieces of bedrock, sediment, derived primarily by mechanical weathering. Clastic rocks may also include chemically weathered sediment. Clastic rocks are classified by grain shape, grain size, and sorting. Chemical sedimentary rocks are precipitated from water saturated with dissolved minerals.CLASTIC VS. CRYSTALLINE TEXTURE. When dealing with rocks, geologists use textural terms to describe rocks as either aggregates of grains, aggregates of crystals, or amorphous. If the rock is made up of an aggregate of interlocking crystals that have grown together in place, the rock has a crystalline texture (Figure 1a). Quartz, Feldspar, Lithics. Color. Reddish brown. Miscellaneous. Angular clasts in a fine- to medium-grained matrix; Immature. Depositional Environment. Alluvial Fan, or Glacial (unstratified till) Type Sedimentary Rock Origin Detrital/Clastic Texture Clastic; Coarse-grained (2 – 64 mm) Composition Quartz, Feldspar, Lithics Color Reddish brown ...Explain the difference between a clastic rock and a crystall | Quizlet Related questions with answers Describe the main light- and dark-colored silicate minerals, including their …6.2 Chemical Sedimentary Rocks. Whereas clastic sedimentary rocks are dominated by components that have been transported as solid clasts (clay, silt, sand, etc.), chemical sedimentary rocks are dominated by components that have been transported as ions in solution (Na +, Ca 2+, HCO 3–, etc.). There is some overlap between the two because ...Breccia is a clastic sedimentary rock made from many different sizes of angular grains, many of which are gravel-sized or larger. These grains are fragments of other rocks, bound together by cement which is typically silica or calcite. Its angular or subangular grains differentiate it from conglomerate. While breccia is a clearly defined rock ...Jun 28, 2012 · TextureDetrital (Clastic Texture)vs.Chemical (Crystalline Texture) Crystalline Texture Coarse Fine Chemical Rock Texture. Clastic Texture Grain Size Grain Sorting Grain Rounding Grain Shape Sediment Maturity Detrital Rock Texture. Grain Size • Gravel2mm • Sand1/16 mm • Mud - Silt1/256 mm • Mud - Clay Igneous rock - Clastic Structures: These are various features that express the accumulation of fragments or the rupturing and dislocation of solid material. In volcanic environments they generally result from explosive activity or the incorporation of solid fragments by moving lava; as such, they characterize the pyroclastic rocks. Among the plutonic rocks, they appear chiefly as local to very ... If non-clastic rocks are fine-grained enough, they too can be called aphanitic. Clastic sedimentary rocks are subdivided on the basis of grain size. Secondary characteristics used to further distinguish clastic rocks are sorting, grain shape, and grain composition. Grain size: Clastic sediments are distinguished on the basis of average grain size.Textures of carbonate rocks are extremely variable. Textures can vary from those similar to clastic sediments, showing characteristic grain sizes, sorting, and rounding, to those produced by chemical precipitation. In carbonates the matrix can range from fine grained carbonate mud to crystalline calcite or dolomite.Sedimentary rock is classified into two main categories: clastic and chemical. Clastic or detrital sedimentary rocks are made from pieces of …Clastic Sedimentary Rocks . Clastic sediments are made of particles of mineral or rock fragments, known as clasts, that have ... Note that there is a relationship between this series and Bowen’s reaction series. The minerals ... (crystalline) Dolomite . Powdered rock reacts with dilute hydrochloric acid (much less reactive than calcite)If non-clastic rocks are fine-grained enough, they too can be called aphanitic. Clastic sedimentary rocks are subdivided on the basis of grain size. Secondary characteristics used to further distinguish clastic rocks are sorting, grain shape, and grain composition. Grain size: Clastic sediments are distinguished on the basis of average grain size.Texture clastic bioclastic crystalline. (3) heat and pressure. (1). (4) melting and/or solidification 1. 2. Rock. A, B, C, D. E. F. (2). Texture. Rock clastic.What is a clastic/detrital sedimentary rock composed entirely of calcite with very fine crystalline, nonclastic texture, that forms in caves is called Dripstone What is an example of a very mature clastic sedimentary rock? CLASTIC VS. CRYSTALLINE TEXTURE. When dealing with rocks, geologists use textural terms to describe rocks as either aggregates of grains, aggregates of crystals, or amorphous. If the rock is made up of an aggregate of interlocking crystals that have grown together in place, the rock has a crystalline texture (Figure 1a). v. Skewness: It is a measure of the degree of symmetry of the size distribution ... Non-clastic texture includes crystalline texture and non-crystalline texture.Crystalline textures include phaneritic, foliated, and porphyritic. Phaneritic textures are where interlocking crystals of igneous rock are visible to the unaided eye. The foliated texture is where metamorphic rock is made of layers of materials. Fragmental textures include clastic, bioclastic, and pyroclastic. Formation:Choose one: A. Clastic sedimentary rocks have larger mineral grains and crystalline igneous rocks have smaller minerals. B. Crystalline igneous rocks are darker in color and clastic sedimentary rocks are lighter. C. Clastic sedimentary rocks contain only one mineral, whereas crystalline igneous rocks contain many minerals. D. Minerals in ...Sedimentation means settling from a fluid, either water or air. The texture of sedimentary rocks is described as "clastic", meaning that they are composed of discrete particles that are compacted and cemented together. An example of a non-clastic texture would be crystalline material. Detrital Sedimentary Rocks. Sediment name. and particle size. 1 Apr 2021 ... These include the rock type (clastic vs. crystalline), the fracture type (shear vs. tensile), the fracture geometry (aperture and roughness) ...How do chemical and biochemical sedimentary rocks form? Lesson 3 - VS. A clastic sedimentary rock is made of clasts of minerals or rock fragments. When ...Crystalline Limestone. When limestone is subjected to heat, pressure, and chemical activity, the calcite in the rock begins to transform. This is the beginning of the process known as metamorphism. Starting at a microscopic scale, the calcium carbonate in the rock begins to crystallize or recrystallize into fine-grained calcite crystals.The sequence in which minerals crystallize from a magma is known as the Bowen reaction series (Figure 3.10 and Who was Bowen). Of the common silicate minerals, olivine normally crystallizes first, at between 1200° and 1300°C. As the temperature drops, and assuming that some silica remains in the magma, the olivine crystals react (combine ...In sedimentary rock: Texture. …groupings exist for sedimentary rocks: clastic (or fragmental) and nonclastic (essentially crystalline). Noncarbonate chemical sedimentary …Clastic definition, breaking up into fragments or separate portions; dividing into parts. See more.Mar 9, 2017 · Clastic rocks are made of particles ranging in size from microscopic to indefinitely large. The rocks with visible clasts are called macroclastic. Extra-large clasts are called phenoclasts—so phenoclasts, phenocrysts and porphyroblasts are cousins. Two sedimentary rocks have phenoclasts: conglomerate and breccia. Sedimentary Textures: Clastic vs. Crystalline Crystals of Calcite and dolomite in carbonate rocks A. Calcite crystals grew into the void space in a limestone, precipitating from calcium and carbonate ions transported in ground water.There are three different types of sedimentary rocks: clastic, organic (biological), and chemical. Clastic sedimentary rocks , like sandstone, form from clasts , or pieces of other rock. Organic sedimentary rocks , like coal, form from hard, biological materials like plants, shells, and bones that are compressed into rock.Sedimentary rocks are commonly grouped according to whether they are clastic, biochemical, or chemical. This works fine, except that it is not clear whether some limestones are biochemical or chemical, and it is not clear where to put dolostone, which is a common rock that often seems to have formed as a result of post-burial chemical alteration of limestone.clastic. shale. clastic. fossiliferous limestone. crystalline, fizzes with acid. Study with Quizlet and memorize flashcards containing terms like sandstone, gypsum, dolostone and more.➢ Clastic (detrital) sedimentary rocks are formed from bits and pieces of ... Crystalline limestone. Bioclastic limestone. Marl; Clastic limestone.Sedimentary rock - Evaporites, Deposits, Minerals: Evaporites are layered crystalline sedimentary rocks that form from brines generated in areas where the amount of water lost by evaporation exceeds the total amount of water from rainfall and influx via rivers and streams. The mineralogy of evaporite rocks is complex, with almost 100 varieties possible, but less than a dozen species are ...Non-Clastic Sedimentary Rock Table; Mineral Chemical Form Characteristics Rock Name; Calcite: CaCO 3: Fizzes in HCl acid: Limestone: Calcite: CaCO 3: Medium to coarse-grained, fizzes in acid: Crystalline Limestone: Calcite: CaCO 3: Microcrystalline, conchoidal fracture, fizzes in acid: Micrite: Calcite: CaCO 3: Aggregates of small round spheres ...Jan 4, 2013 · Sedimentary rocks are classified based on how they form and on the size of the sediments, if they are clastic. Clastic sedimentary rocks are formed from rock fragments, or clasts; chemical sedimentary rocks precipitate from fluids; and biochemical sedimentary rocks form as precipitation from living organisms. Practice Cementation refers to the chemical precipitation of new minerals between pre-existing grains which helps to bind or cement the grains together. The most common cements are calcite (CaCO 3) and silica (quartz, SiO 2 ), but hematite (Fe 2 O 3) and limonite [FeO (OH)] may also occur. 3. Re-crystallization may occur, in which the existing minerals ...See answer (1) Best Answer. Copy. A Clastic sedimentary rock forms when fragments of preexisting rocks are compacted or cemented together. A Bioclastic rock is a clastic rock but the fragments are ...Describe the differences between cobbles, pebbles, sand, silt, and clay and explain the relationship between clast size and the extent to which clasts can be transported by moving water or by wind. Describe the characteristics of the various types of clastic sedimentary rock, including the significance of differences in the composition of ...A mineral is a naturally occurring, inorganic solid with a definite chemical composition and a crystalline structure formed by geological processes. A rock is an aggregate of one or more minerals whereas a rock may also include organic remains and mineraloids. Some rocks are predominantly composed of just one mineral.The difference between crystal and crystalline is that Crystal refers to a specific kind of rock, constituted of atoms and well structured in all spatial directions. At the same time, the rocks that possess crystal qualities, characteristics, and properties are called crystalline.Clastic Texture vs. Crystalline Texture. Expert Answer. Who are the experts? Experts are tested by Chegg as specialists in their subject area. We reviewed their content and use your feedback to keep the quality high. The structure of the rocks is the size, shape and arrangements of crystals or grains .Sedimentary rocks are classified based on how they form and on the size of the sediments, if they are clastic. Clastic sedimentary rocks are formed from rock fragments, or clasts; chemical sedimentary rocks precipitate from fluids; and biochemical sedimentary rocks form as precipitation from living organisms. PracticeThey consist of 50 percent or more calcite and aragonite (both CaCO3). Dolomites are mainly produced by the secondary alteration or replacement of limestones; i.e., the mineral dolomite [CaMg (CO3)2] replaces the calcite and aragonite minerals in limestones during diagenesis.In sedimentary rock: Texture. …groupings exist for sedimentary rocks: clastic (or fragmental) and nonclastic (essentially crystalline). Noncarbonate chemical sedimentary …Sedimentary Rocks with clastic textures – may contain some igneous minerals, but also non-igneous minerals (e.g., clay). Sedimentary Rocks with crystalline textures – composed of minerals not common in igneous rocks. Foliated Metamorphic Rocks: distinguished from igneous and sedimentary rocks by foliation. Some contain minerals only found ... sedimentary rock. Sedimentary rock - Iron-Rich, Clastic, Chemical: Almost all sedimentary rocks are iron-bearing in the sense that mudrocks, sandstones, and carbonates typically have an iron content of several percent. Nevertheless, sedimentary rocks in which the proportion of iron exceeds 15 percent are separately categorized as iron-rich. Two ... Sedimentary Rocks with clastic textures – may contain some igneous minerals, but also non-igneous minerals (e.g., clay). Sedimentary Rocks with crystalline textures – composed of minerals not common in igneous rocks. Foliated Metamorphic Rocks: distinguished from igneous and sedimentary rocks by foliation. Some contain minerals only found ... Textures of carbonate rocks are extremely variable. Textures can vary from those similar to clastic sediments, showing characteristic grain sizes, sorting, and rounding, to those produced by chemical precipitation. In carbonates the matrix can range from fine grained carbonate mud to crystalline calcite or dolomite. Adjective (en adjective) (geology) Consisting of, or pertaining to, geological detritus. * {{quote-book, 1964, N.D. Bespalov, Soils of Outer Mongolia, page=172 citation; passage=The light-chestnut soils are much more detrital than the chestnut varieties — not only at the surface but throughout the soil strata, except on sandy tracts.1. solid. 2. naturally occurring, found on/in earth. 3. inorganic substance. 4. specific arrangement of atoms (crystalline structure) 5. Salt - NaCl - halite specific chemical composition. Explain the difference between a mineral in a vitamin pill and a geologic mineral. A vitamin pill is not a naturally occurring mineral, as it has been ...focus a beam of electrons on a small part of a grain to produce a signal that defines a chemical composition of the mineralClastic sedimentary rocks are formed by an accumulation of weathered fragments of other rocks that have hardened with a matrix material. Take a look at the picture below. Take a look at the ...Clastic sedimentary rocks are formed by an accumulation of weathered fragments of other rocks that have hardened with a matrix material. Take a look at the picture below. Take a look at the ...Medium-grained rocks can be composed of quartz grains, feldspar grains (arkose), or rock fragments and clay (graywacke). Medium-sized grains in clastic sedimentary rocks form sandstone. This sample is a quartz sandstone. • Fine-grained (<1/16 mm) rocks are generally called mudrocks. They include siltstone and shale.Crystalline rock, any rock composed entirely of crystallized minerals without glassy matter. Intrusive igneous rocks—those that congeal at depth—are virtually always crystalline, whereas extrusive igneous rocks, or volcanic rocks, may be partly to entirely glassy. Many factors influence the. 6 Mei 2022 ... Microbial Diversity in Caves: Microbe, v. 2, p. 132-138. Bosch, R. F., and White, W. B., 2004, Lithofacies and transport of clastic sediments in ...Sedimentary rocks are formed by the lithification of inorganic and/or organic sediments, or as chemical precipitates. There are two types of sedimentary rocks: Clastic and Chemical Clastic sedimentary rocks form when existing parent rock material is weathered, fragmented, transported, and deposited in layers that compact,The photo seen here (Figure 7.25) shows a marble made of coarsely crystalline calcite. ... Many chemical sedimentary rocks contain clastic material, and many ...There are four distinct kinds of sedimentary rocks: clastic, biochemical, organic and chemical. Clastic sedimentary rocks are also called detrital , and they form as a result of accumulation of rock fragments. Classified on the basis of particle size and texture, examples of clastic sedimentary rocks include mudstone, siltstone and sandstone.v. Skewness: It is a measure of the degree of symmetry of the size distribution ... Non-clastic texture includes crystalline texture and non-crystalline texture.Sedimentary rocks are classified based on how they form and on the size of the sediments, if they are clastic. Clastic sedimentary rocks are formed from rock fragments, or clasts; chemical sedimentary rocks precipitate from fluids; and biochemical sedimentary rocks form as precipitation from living organisms. PracticeStudy 8.1 The Coastal Zone flashcards from Gina Elliott's class online, or in Brainscape's iPhone or Android app. Learn faster with spaced repetition.Chert is also the name given to hard sedimentary rock composed of fine quartz crystals. The rock seen in Figure 7.75 is an example. The rock seen in Figure 7.75 is an example. Chert (the rock) is usually of biological origin, being the petrified remains of siliceous ooze, the biogenic sediment that covers large areas of the deep ocean floor.18 Nov 2015 ... Sedimentary rocks, lithification, compaction and cementation, clastic vs. nonclastic sedimentary rocks. Conglomerates, sandstones, and ...The main petrology is micrite-silt crystal-sized dolomite, fine-to-medium crystalline algal dolomite, muddy dolomite, limy dolomite, ... current direction and clastic supply. At the time of maximum regression the shoal was emergent and subjected to fresh-water leaching. A final regressive phase covered the area with foraminiferal micrite facies ...Crystalline, Clastic, Bioclastic, Oolitic, Etc. Composition of Major Fraction: Composition as Indicated in left column (prefix appropriate names for mixtures) Chiefly Calcite or Dolomite: Composition of Minor Fraction < 10% Minor Fraction : Limestone, Dolomite, Etc.: All varieties in the Calcite-Dolomite horizontal column are possibe here.Sedimentary rock - Clastic, Chemical, Organic: Conglomerates and breccias are sedimentary rocks composed of coarse fragments of preexisting rocks held together either by cement or by a finer-grained clastic matrix. Both contain significant amounts (at least 10 percent) of coarser-than-sand-size clasts. Breccias are consolidated rubble; their clasts are angular or subangular. Conglomerates are ... Answer to: What is the difference between clastic (detrital) and chemical/biochemical sedimentary rocks? By signing up, you'll get thousands of... Log In. Sign Up. Menu. ... What are the texture (clastic, crystalline, or bioclastic), particle size if clastic (various, sand (0.006 - 0.2 cm), silt (0.0004 - 0.006 cm), or clay (less than 0.0004 cm ...by Jamey T Sedimentary rocks are comprised of varying sizes of grains of rock or organic fragments which are called sediment. They are set apart into three different types of sedimentary rock; clastic, biogenic, and chemical. These types of sedimentary rocks are made different by the way they are formed and their composition.Crystals begin to form if the ions present within a fluid, such as water, become very concentrated, either by the addition of more ions or the removal of water by freezing or evaporation. ... 4.3.1 Clastic Sedimentary Rocks. Weathering and erosion occur normally in areas that are at high elevation, such as mountains, while deposition occurs in ...Amorphous solids. Solids which particles are not arranged in a regular pattern. Examples of amorphous solids. Plastics rubber, glass. What is a difference between them in terms of temperature? Amorphous solids do not melt at a distinct temp, like crystalline solids. Instead, they just become softer and softer or change into another substance.sedimentary rock. Sedimentary rock - Iron-Rich, Clastic, Chemical: Almost all sedimentary rocks are iron-bearing in the sense that mudrocks, sandstones, and carbonates typically have an iron content of several percent. Nevertheless, sedimentary rocks in which the proportion of iron exceeds 15 percent are separately categorized as iron-rich. Two ... There are three main types of rocks: sedimentary, igneous, and metamorphic. Each of these rocks are formed by physical changes—such as melting, cooling, eroding, compacting, or deforming —that are part of the rock cycle. Sedimentary Rocks Sedimentary rocks are formed from pieces of other existing rock or organic material. There are three different types of sedimentary rocks: clastic ...Limestone Rocks on the Beach. Texture: Clastic or Non-Clastic. Grain size: Variable, can consist of clasts of all sizes. Hardness: Generally hard. Major minerals: Calcite, dolomite. Composition: Limestone consists primarily of calcium carbonate, but it may also contain variable amounts of impurities such as clay, silt, and organic …Clastic or detrital sedimentary rocks are made from pieces of bedrock, sediment, derived primarily by mechanical weathering. Clastic rocks may also include chemically weathered sediment. Clastic rocks are classified by grain shape, grain size, and sorting. Chemical sedimentary rocks are precipitated from water saturated with dissolved minerals.9.0.2 Four Types of Sedimentary Rocks. Sedimentary rocks can be divided into four main types: clastic, chemical, biochemical, and organic. Clastic sedimentary rocks are composed mainly of material that is transported as solid fragments (called clasts), and then cemented together by minerals that precipitated from solution.Answer to: Complete the chart with the texture (clastic, crystalline, or bioclastic), grain size (various sizes, sand, silt, clay, fine to course,...Answer to: What is the difference between clastic (detrital) and chemical/biochemical sedimentary rocks? By signing up, you'll get thousands of... Log In. Sign Up. Menu. ... What are the texture (clastic, crystalline, or bioclastic), particle size if clastic (various, sand (0.006 - 0.2 cm), silt (0.0004 - 0.006 cm), or clay (less than 0.0004 cm ...Adult Education. Basic Education. High School Diploma. High School Equivalency. Career Technical Ed. English as 2nd Language.
Two main natural textural groupings exist for sedimentary rocks: clastic (or fragmental) and nonclastic (essentially crystalline). Noncarbonate chemical sedimentary rocks in large part exhibit crystalline texture, with individual …. Kansas jayhawks men's basketball transfer
What are the 5 critrias to classify a mineral? 1. Solid 2. Inorganic 3. Orderly arrangment of atoms 4.Naturaly occurring not man made 5. Fixed chemical (formula recipe) What are the 6 cyrstal systems. 1.Cubic 2.Aug 28, 2022 · 1.22 Opal. Opal contains silicon and oxygen. It has about the same composition as quartz but contains up to 10% water. On an atomic scale, opal is not crystalline; it comprises spheres of silica (SiO 2 ), 150-300 nanometers in diameter, arranged in a random pattern. Chemical Sedimentary Rocks. Sedimentary rocks formed by the crystallization of chemical precipitates are called chemical sedimentary rocks. Dissolved ions in fluids precipitate out of the fluid and settle out, just like the halite pictured below ( Figure below). The evaporite, halite, on a cobble from the Dead Sea, Israel.Clastic sedimentary rocks are composed of fragments (clasts) of pre-existing rock. Siliciclastic sedimentary rocks are composed predominantly of clasts of silicate minerals, of which quartz and feldspar are usually most common. ... Intercrystalline porosity is the space present between crystals in a rock and is usually secondary.Foliated (Banded) Metamorphic Rocks. In this texture, the mineral crystals in the rock are aligned with each other. This alignment may be displayed as parallel planes along which the rock splits, by overlapping sheets of platy minerals such as micas, by the parallel alignment of elongate minerals such as amphiboles, or by alternating layers of light and dark minerals.Chemical Sediment - Components were dissolved, transported in solution, and precipitated chemically. This sediment contains no clastic particles. Types of Chemical Sedimentary Rocks - Rock Salt (Halite), Gypsum, Chert (silica). Mineral Deposits include iron and phosphorus deposits) Biogenic Sediment - a sediment composed mainly of fossil remains.View Notes - Geology Test Review from GEOL 1121K at Georgia State University. Test Review: Chapter 1: - Formation of universe - Age of universe - Age of earth - Heliocentric vs. geocentric model -A mineral is a naturally occurring, inorganic solid with a definite chemical composition and a crystalline structure formed by geological processes. A rock is an aggregate of one or more minerals whereas a rock may also include organic remains and mineraloids. Some rocks are predominantly composed of just one mineral. Chemical Sediment - Components were dissolved, transported in solution, and precipitated chemically. This sediment contains no clastic particles. Types of Chemical Sedimentary Rocks - Rock Salt (Halite), Gypsum, Chert (silica). Mineral Deposits include iron and phosphorus deposits) Biogenic Sediment - a sediment composed mainly of fossil remains.The photo seen here (Figure 7.25) shows a marble made of coarsely crystalline calcite. ... Many chemical sedimentary rocks contain clastic material, and many ...Texture: Non-clastic sedimentary rock. Grain size: Cryptocrystalline, cannot be seen except under very high magnification. Hardness: Hard. ... Chert is as hard as crystalline quartz with a hardness rating of seven in the Mohs scale — maybe a bit softer, 6.5, if it still has some hydrated silica in it. Beyond simply being hard, chert is a ...COLOR to distinguisj minerals.) Silicates – most common mineral group Some gem minerals - Turqoise, Feldspar, Diamond Rocks clastic vs crystalline; igneous metamorphic and sedimentary Rock Cycle – Igneous rocks and environments (ch 05) Atomic structure of solids, liquids and gases – Decompression melting Hydrous melting Partial melting …They consist of 50 percent or more calcite and aragonite (both CaCO3). Dolomites are mainly produced by the secondary alteration or replacement of limestones; i.e., the mineral dolomite [CaMg (CO3)2] replaces the calcite and aragonite minerals in limestones during diagenesis..