This efflorescent example by the effervescent Sam Ezersky doesn't disappoint.
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Where the artist added an iridescent glaze, the shapes are transformed into efflorescent flora and fauna that appear to concomitantly expand and contract.
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She put together the hardy and the delicate and the efflorescent in a way that no one had before, and just like that, the world shifted.
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"You can have the most advanced and efflorescent of cultures," he wrote in the introduction to his memoir, "Things That Matter: Three Decades of Passions, Pastimes and Politics" (21990).
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It isn't clear if Efflorescent 1 is hard or soft to the touch: A solid wall slowly seems to be turning into an elastic, wrinkled patch of skin, or a giant plastic bag.
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Pupa efflorescent. The larvae feed on Phyllanthus and Sauropus species.
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Pupa efflorescent. The larvae feed on Phyllanthus and Sauropus species.
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His Benedick, the best I have seen, was hilarious and heart-breaking, vain, masculine, silly and romantically efflorescent.
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Pupa efflorescent. The larvae feed on Cytisus, Desmodium, Wisteria, Arachis, Butea, Cajanus, Calopogonium, Crotalaria, Derris, Glycine, Indigofera, Mucuna, Phaseolus, Pueraria, Rhynchosia, Tephrosia, Vigna, Shorea, Hevea, Gossypium, Nephelium and Solanum species.
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Raichur Junction railway station (station code:RC), is located in Raichur district in the Indian state of Karnataka and serves Raichur and the surrounding industrially efflorescent area. The station has three platforms.
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It may occur as fibrous, granular, lamellar, or compact. A fibrous, efflorescent form is known as lublinite. Cleavage is usually in three directions parallel to the rhombohedron form. Its fracture is conchoidal, but difficult to obtain.
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Rio Tinto in Spain. Water temperatures as high as 47 °CNordstrom, D.K. & Alpers, C. N.: Negative pH, efflorescent mineralogy, and consequences for environmental restoration at the Iron Mountain Superfund site, California PNAS, vol. 96 no. 7, pp 3455–3462, 30 March 1999.
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Zippeite is a hydrous potassium uranium sulfate mineral with formula: K4(UO2)6(SO4)3(OH)10·4(H2O). It forms yellow to reddish brown monoclinic- prismatic crystals with perfect cleavage. The typical form is as encrustations and pulverulent earthy masses. It forms as efflorescent encrustations in underground uranium mines.
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Since the closing of the Markey mine, oxidation of primary ores in the humid underground environment has produced a variety of secondary minerals. These secondary minerals are primarily sulfates as efflorescent crusts on the surfaces of mine walls. It is found on calcite-veined asphaltum in association with gypsum, markeyite, and rozenite.
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It is commonly found as translucent small rhombohedral crystals that have angles close to 90 degrees although its crystal system is nominally trigonal. Its Mohs hardness is 2.5, with an average specific gravity of 2.8. It occurs in the oxidized zone of uranium-bearing polymetallic ore deposits. It also may occur as an efflorescent crust on the walls and timbers of uranium mines.
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Sodium thiosulfate (sodium thiosulphate) is an inorganic compound with the formula Na2S2O3.H2O. Typically it is available as the white or colorless pentahydrate, Na2S2O3·5H2O. The solid is an efflorescent (loses water readily) crystalline substance that dissolves well in water. Sodium thiosulfate is used in gold mining, water treatment, analytical chemistry, the development of silver-based photographic film and prints, and medicine.
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Johannite is a rare uranium sulfate mineral. It crystallizes in the triclinic crystal system with the chemical composition Cu[UO2(OH)SO4]2·8H2O. It crystallizes in the triclinic system and develops only small prism or thin to thick tabular crystals, usually occurs as flaky or spheroidal aggregates and efflorescent coatings. Its color is emerald-green to apple-green and its streak is pale green.
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Niter is a colorless to white mineral crystallizing in the orthorhombic crystal system. It usually is found as massive encrustations and efflorescent growths on cavern walls and ceilings where solutions containing alkali potassium and nitrate seep into the openings. It occasionally occurs as prismatic acicular crystal groups, and individual crystals commonly show twinning. Niter and other nitrates can also form in association with deposits of guano and similar organic materials.
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Lake Logipi has a maximum depth of 3 to 5 m, and is about 6 km wide by 3 km long. Its waters are of sodium bicarbonate composition with a pH of 9.5-10.5 and salinity (total dissolved salts) that varies from less than 20 g/l to greater than 50 g/l. Efflorescent salt crusts (trona) are present around its margins. Flamingoes frequently inhabit the saline waters feeding on cyanobacteria (Arthrospira spp.
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Peloidal or efflorescent massive mudstone is similar to brecciated massive mudstone, but its mud fragments are small, rounded clumps. This clumping pattern resembles that of modern salty playas, where dissolved salt gives the lakebed mud a crumbly powdered texture. Traces of mudcracks are still present, but have been heavily deformed by the textural changes. The wettest type of massive mudstone is burrowed massive mudstone, which is thin- bedded mudstone that has been completely homogenized by bioturbation.
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