Natural materials

thumb|upright=1.25|Surface-water-Gley soil|gley developed in [[glacial till in Northern Ireland]]

thumb|upright=1.25|Crystals of serandite, [[natrolite, analcime, and aegirine from Mont Saint-Hilaire, Quebec, Canada]]

Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolinite, ). Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impurities, such as a reddish or brownish colour from small amounts of iron oxide.

thumb|Bundles of rice straw thumb|Pile of stacked small rectangular straw bales sheltered under a clear tarpaulin thumb|Straw lines and a Combine Harvester|combine harvester Straw is an agricultural byproduct consisting of the dry stalks of cereal plants after the grain and chaff have been removed. It makes up about half of the yield by weight of cereal crops such as barley, oats, rice, rye and wheat. It has a number of different uses, including fuel, livestock bedding and fodder, thatching and basket making.

thumb|upright=1.35|Gravel (largest fragment in this photo is about )

thumb|upright=1.35|Close view of pebbles

thumb|A schist showing characteristic scaly schistose texture caused by platy mica|micas Schist ( ) is a medium-grained metamorphic rock generally derived from fine-grained sedimentary rock, like shale. It shows pronounced schistosity (named for the rock). This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture reflects a high content of platy minerals, such as mica, talc, chlorite, or graphite. These are often interleaved with more granular minerals, such as fel

Slate is a fine-grained, foliated, homogeneous, metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade, regional metamorphism. It is the finest-grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression.

polymers of the organic compound isoprene, with minor impurities of other organic compounds; refined from latex harvested from rubber trees

thumb|This Balancing rock|balancing boulder, "[[Balanced Rock", stands in Garden of the Gods park in Colorado Springs, Colorado, United States.]] thumb|Boulder in British Columbia, Canada thumb|Kämmenkivi stone on the Pisa hill in Kuopio, Finland thumb|Balanced granite boulders at Hyderabad, India In geology, a boulder is a rock fragment with size greater than in diameter. Smaller pieces are called cobbles and pebbles. While a boulder may be small enough to move or roll manually, others are extremely massive. In common usage, a boulder is too large for a person to move. Smaller boulders are us

mortarless masonry method

thumb|right|A thatched public house|pub (The Williams Arms) at [[Wrafton, North Devon, England]] Thatching is the craft of building a roof with dry vegetation such as straw, water reed, sedge (Cladium mariscus), rushes, heather, or palm branches, layering the vegetation so as to shed water away from the inner roof. Since the bulk of the vegetation stays dry and is densely packed—trapping air—thatching also functions as insulation. It is a very old roofing method and has been used in both tropical and temperate climates. Thatch is still employed by builders in developing countries, usually with

substrate suitable for hydroculture applications

artificial gravel of angular shape, used as construction aggregate

technique for constructing foundations, floors, and walls by compacting a damp mixture of sub soil

thumb|Cobblestones on a road surface in Imola, Italy thumb|upright|Sett (paving)|Sett-paving, such as this surface in [[Fulham, south-west London, is also often referred to as "cobblestones".]]

Rubble is broken stone, of irregular size, shape and texture; undressed especially as a filling-in. Rubble naturally found in the soil is known also as 'brash' (compare cornbrash). Where present, it becomes more noticeable when the land is ploughed or worked.

fibre obtained from the phloem tissues of many plants, used for textiles, rope, and paper

any fibre derived from natural sources such as plants, animals or minerals

species of plant

substance produced by life processes; it may be either constituents, or secretions, of plants or animals

natural building material made from subsoil, water, some kind of fibrous organic material (typically straw)

natural mixture of hydrated silicate clays colored with red iron oxide

masonry structural division

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thumb|300px|Cross-section of a gas mask filter, with sorbent material visible A sorbent is an insoluble material that either absorbs or adsorbs liquids or gases. They are frequently used to remove pollutants and in the cleanup of chemical accidents and oil spills. Besides their uses in industry, sorbents are used in commercial products such as diapers and odor absorbents, and are researched for applications in environmental air analysis, particularly in the analysis of volatile organic compounds. The name sorbent is derived from sorption, which is itself a derivation from adsorption and absorp

building material

thumb|A pollarding|pollarded willow with a crop of withies ready for harvest thumb|Cutting and stacking withies thumb|upright|Drying withies A withy or withe (also willow and osier) is a strong flexible willow stem, typically used in thatching, basketmaking, gardening and for constructing woven wattle hurdles. The term is also used to refer to any type of flexible rod of natural wood used in rural crafts such as hazel or ash created through coppicing or pollarding.

product or physical matter that arises without the use of technology

thumb|Flintknapping a stone tool

Trass is the local name of a volcanic tuff occurring in the Eifel, where it is worked for hydraulic mortar. It is a grey or cream-coloured fragmental rock, largely composed of pumiceous dust, and may be regarded as a trachytic tuff. It much resembles the Italian pozzolana and is applied to like purposes. Mixed with lime and sand, or with Portland cement, it is extensively employed for hydraulic work, especially in the Netherlands; while the compact varieties have been used as a building material and as a fire-stone in ovens. Trass was formerly worked extensively in the Brohl valley and is now

Wood product from a responsibly managed forest

craft material of metal particles and a plastic binder

Heterogenite is a natural tri-valent cobalt oxyhydroxide mineral. It is the most abundant oxidised cobalt mineral in the Katanga Copperbelt, a region in the Democratic Republic of the Congo. About 70% of known heterogenite is located in the DRC.

any material that originates from living organisms

Ikranite is a member of the eudialyte group, named after the Shubinov Institute of Crystallography of the Russian Academy of Sciences. It is a cyclosilicate mineral that shows trigonal symmetry with the space group R3m, and is often seen with a pseudo-hexagonal habit. Ikranite appears as translucent and ranges in color from yellow to a brownish yellow. This mineral ranks a 5 on Mohs scale of mineral hardness, though it is considered brittle, exhibiting conchoidal fracture when broken.

Grayite, ThPO4·(H2O), is a thorium phosphate mineral of the Rabdophane group first discovered in 1957 by S.H.U. Bowie in Rhodesia. It is of moderate hardness occurring occasionally in aggregates of hexagonal crystals occasionally but more commonly in microgranular/cryptocrystalline masses. Due to its thorium content, grayite displays some radioactivity although it is only moderate and the mineral displays powder XRD peaks without any metamict-like effects. The color of grayite is most commonly observed as a light to dark reddish brown but has also been observed as lighter yellows with grayish

Dorrite is a silicate mineral that is isostructural to the aenigmatite group. It is most chemically similar to the mineral rhönite [Ca2Mg5Ti(Al2Si4)O20], made distinct by a lack of titanium (Ti) and the presence of Fe3+. Dorrite is named for Dr. John (Jack) A. Dorr, a late professor at the University of Michigan that researched in outcrops where dorrite was found in 1982. This mineral is sub-metallic resembling colors of brownish-black, dark brown, to reddish brown.

thumb | right Takedaite is a borate mineral that was found in a mine in Fuka, Okayama Prefecture Japan during a mineralogical survey in the year 1994. During the survey, Kusachi and Henmi reported the occurrence of an unidentified anhydrous borate mineral closely associated with nifontovite, olshanskyite, and calcite. By the year 1994 two other minerals in the borate group M3B2O6 had been identified in nature Mg3B2O6 known as kotoite and Mn3B2O6 known as jimboite. Takedaite has the ideal chemical formula of Ca3B2O6. The mineral has been approved by the Commission on New Minerals and Mineral Na

Nevadaite is a rare phosphate mineral with a chemical formula of {| |Cu2Zn0.02V3+0.98Al1.15Al8P7.9O32F8.37(OH)1.63(H2O)21.65 |- |}

important raw materials

Allendeite, Sc4Zr3O12, is an oxide mineral. Allendeite was discovered in a small ultrarefractory inclusion within the Allende meteorite. This inclusion has been named ACM-1. It is one of several scandium rich minerals that have been found in meteorites. Allendeite is trigonal, with a calculated density of 4.84 g/cm3. The new mineral was found along with hexamolybdenum. These minerals, are believed to demonstrate conditions during the early stages of the Solar System, as is the case with many CV3 carbonaceous chondrites such as the Allende meteorite. It is named after the Allende meteorite

smaller chunks or particles of granite, produced by weathering

Scotlandite is a sulfite mineral first discovered in a mine at Leadhills in South Lanarkshire, Scotland, an area known to mineralogists and geologists for its wide range of different mineral species found in the veins that lie deep in the mine shafts. This specific mineral is found in the Susanna vein of Leadhills, where the crystals are formed as chisel-shaped or bladed. Scotlandite was actually the first naturally occurring sulfite, which has the ideal chemical formula of PbSO3. The mineral has been approved by the Commission on New Minerals and Mineral Names, IMA, to be named scotlandite fo

Dessauite-(Y) is a mineral member of the crichtonite group with the formula . It is associated with derbylite, hematite, rutile, karelianite, siderite, and calcite. Founded in the Buca della Vena Mine, Tuscany, Italy, the mineral was called dessauite in honor of professor Gabor Dessau (1907–1983).

Simmonsite is a halide mineral, being a tertiary light metal fluoride, with formula Na2LiAlF6. It was first discovered in nature in Mineral County in the Gillis Range of Nevada, U.S.A. The mineral is found intergrown with cryolite, cryolithionite and trace elpasolite. The mineral has a monoclinic structure of P2 or P2/m. The ideal chemical formula for simmonsite is Na2LiAlF6. The mineral has a no visible cleavage, Mohs hardness of 2.53, a pale white color with a white streak and feels somewhat greasy. Simmonsite was named for the Professor of Mineralogy and Petrology at the University of New O