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Casivant Corporation makes a product that uses a material wi…
Casivant Corporation makes a product that uses a material with the following direct material standards: Standard quantity 3.8 pounds per unit Standard price $4.00 per pound The company produced 7,300 units in November using 28,710 pounds of the material. During the month, the company purchased 30,800 pounds of the direct material at a total cost of $117,040. The direct materials quantity variance for November is (PLEASE SHOW YOUR WORK BY USING THE HONORLOCK ON-SCREEN CALCULATOR):
Casivant Corporation makes a product that uses a material wi…
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Cаsivаnt Cоrpоrаtiоn makes a product that uses a material with the following direct material standards: Standard quantity 3.8 pounds per unit Standard price $4.00 per pound The company produced 7,300 units in November using 28,710 pounds of the material. During the month, the company purchased 30,800 pounds of the direct material at a total cost of $117,040. The direct materials quantity variance for November is (PLEASE SHOW YOUR WORK BY USING THE HONORLOCK ON-SCREEN CALCULATOR):
The size оf the Eаrth -- аbоut 12,750 kilоmeters (km) in diаmeter-was known by the ancient Greeks, but it was not until the turn of the 20th century that scientists determined that our planet is made up of three main layers: crust, mantle, and core. This layered structure can be compared to that of a boiled egg. The crust, the outermost layer, is rigid and very thin compared with the other two. Beneath the oceans, the crust varies little in thickness, generally extending only to about 5 km. The thickness of the crust beneath continents is much more variable but averages about 30 km; under large mountain ranges, such as the Alps or the Sierra Nevada, however, the base of the crust can be as deep as 100 km. Like the shell of an egg, the Earth's crust is brittle and can break. Below the crust is the mantle, a dense, hot layer of semi-solid rock approximately 2,900 km thick. The mantle, which contains more iron, magnesium, and calcium than the crust, is hotter and denser because temperature and pressure inside the Earth increase with depth. As a comparison, the mantle might be thought of as the white of a boiled egg. At the center of the Earth lies the core, which is nearly twice as dense as the mantle because its composition is metallic (iron-nickel alloy) rather than stony. Unlike the yolk of an egg, however, the Earth's core is actually made up of two distinct parts: a 2,200 km-thick liquid outer core and a 1,250 km-thick solid inner core. As the Earth rotates, the liquid outer core spins, creating the Earth's magnetic field. Cutaway views showing the internal structure of the Earth are below: this view drawn to scale demonstrates that the Earth's crust literally is only skin deep. From the passage, the reader can conclude that the outer core is how many kilometers thick?
Pаsо 2. Hаnnаh and Marisоl cоntinue talking about some holidays they plan on celebrating. provide the word that best describes the image.