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Geology of Morocco. The geology of Morocco formed beginning up to two billion years ago, in the Paleoproterozoic and potentially even earlier. It was affected by the Pan-African orogeny, although the later Hercynian orogeny produced fewer changes and left the Maseta Domain, a large area of remnant Paleozoic massifs.
Moroccanoil is an Israeli [2] [3] cosmetics company headquartered in New York City, [4] [5] [6] specializing in hair care products containing argan oil. The company was founded in 2008 in Montreal by Chilean-Canadian Carmen Tal and her Israeli then-husband Ofer Tal.
An example of conglomerate can be seen at Montserrat, near Barcelona. Here, erosion has created vertical channels that give the characteristic jagged shapes the mountain is named for (Montserrat literally means "jagged mountain"). The rock is strong enough to use as a building material, as in the Santa Maria de Montserrat Abbey.
Bentonite – Rock type or absorbent swelling clay; Brisbane tuff; Eutaxitic texture – Layered or banded texture in some extrusive rock bodies; Sillar – Variety of rhyolite containing fragments of andesite; Tuffite – Tuff containing both pyroclastic and detrital materials; Ignimbrite – Type of volcanic rock, a type of welded tuff.
Rhassoul, or ghassoul (Moroccan Arabic: الغاسول, romanized: l-ġasul), is a cosmetic made of natural mineral clay mined from the Atlas Mountains of Morocco. It is mixed with water, sometimes with herbs or other substances, to clean the body. It has been used by Moroccan women on their skin and hair for centuries.
Soil texture is a classification instrument used both in the field and laboratory to determine soil classes based on their physical texture. Soil texture can be determined using qualitative methods such as texture by feel, and quantitative methods such as the hydrometer method based on Stokes' law .
Soil types by clay, silt and sand composition as used by the United States Department of Agriculture. Loam (in geology and soil science) is soil composed mostly of sand (particle size > 63 micrometres (0.0025 in)), silt (particle size > 2 micrometres (7.9 × 10 −5 in)), and a smaller amount of clay (particle size < 2 micrometres (7.9 × 10 −5 in)).
Ultisol, commonly known as red clay soil, is one of twelve soil orders in the United States Department of Agriculture soil taxonomy. The word "Ultisol" is derived from "ultimate", because Ultisols were seen as the ultimate product of continuous weathering of minerals in a humid, temperate climate without new soil formation via glaciation .
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