It is 21/23.
To find the lateral surface area of a hexagonal prism, first calculate the perimeter of the hexagonal base (P) by adding the lengths of all six sides. Then, multiply the perimeter by the height (h) of the prism using the formula: Lateral Surface Area = P × h. This gives you the area of the sides of the prism that connect the two hexagonal bases.
The surface area to volume ratio decreases - assuming the shape remains similar.
To find the surface area of the smaller figure, we can use the relationship between the volumes and surface areas of similar figures. The volume ratio of the larger figure to the smaller figure is ( \frac{2744}{729} = \left(\frac{a}{b}\right)^3 ), where ( a ) is the linear dimension of the larger figure and ( b ) is that of the smaller figure. Taking the cube root gives the linear scale factor ( \frac{a}{b} = \frac{14}{9} ). The surface area ratio, which is the square of the scale factor, is ( \left(\frac{14}{9}\right)^2 = \frac{196}{81} ). Given the surface area of the larger figure is 392 mm², the surface area of the smaller figure is ( 392 \times \frac{81}{196} = 162 ) mm².
First divide the pineapple by 43 and then multiply by 9 then subtract 2 and there you go good luck ;D
It can be.
Hexagonal tessellation is covering a plane surface with multiple copies of a hexagon.
you dont
The surface area to volume ratio decreases - assuming the shape remains similar.
you put: a squared over b squared = surface area of the smaller solid over surface area of the bigger solid
An isotropic surface is the optimal environment for central colonization, therefore creating a perfect distribution of regular hexagonal patterns.
Hexagonal tessellation is covering a plane surface with multiple copies of a hexagon.
Hexagonal prisms cannot be regular. If you tried to make one it would end up being a hexagon since six equilateral triangles make a hexagon. Therefore, there is no surface area.
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An extrusive igneous rock with a composition similar to granite but with smaller crystals is called rhyolite. Rhyolite forms from the rapid cooling of magma at the Earth's surface, resulting in fine-grained crystals. It is light in color and rich in silica, similar to granite.
A DIP holder or a small outline IC
To find the surface area of the smaller figure, we can use the relationship between the volumes and surface areas of similar figures. The volume ratio of the larger figure to the smaller figure is ( \frac{2744}{729} = \left(\frac{a}{b}\right)^3 ), where ( a ) is the linear dimension of the larger figure and ( b ) is that of the smaller figure. Taking the cube root gives the linear scale factor ( \frac{a}{b} = \frac{14}{9} ). The surface area ratio, which is the square of the scale factor, is ( \left(\frac{14}{9}\right)^2 = \frac{196}{81} ). Given the surface area of the larger figure is 392 mm², the surface area of the smaller figure is ( 392 \times \frac{81}{196} = 162 ) mm².