Rectangle j'k'l'm' shown on the grid is the image of rectangle jklm after transformation. the same transformation will be applied on trapezoid stuv. rectangle jklm is drawn on the grid with vertices j at negative 7, negative 6. k is at negative 4, negative 6. l is at negative 4, negative 2. m is at negative 7, negative 2. rectangle j prime k prime l prime m prime is drawn with vertices j at prime 6, negative 9. k prime is at 9, negative 9. l prime 9, negative 5. m prime is at 6, negative 5. trapezoid stuv is drawn with vertices at s 3, 2. t is at 5, 5. u is at 2, 6. v is at 1, 4. what will be the location of t' in the image trapezoid s't'u'v'? (18, −2) (18, 2) (15, −2) (15, 2)

the answer is:

the lateral area is equal to

to find the lateral area of the square pyramid, first we need to find the perimeter of the base, and then, find the lateral area using the following formulas:

where,

s, is the base length

slant height, is the height of a the side of the pyramid

we are given:

now, calculating the perimeter of the base, we have:

then, calculating the lateral area:

hence, we have that the lateral area is equal to

have a nice day!

cool stunts are flippin i think

sitting on a chair

and using stick feet

large crystals result from very slow cooling.

evaporation of water: this would produce an evaporite which is a sedimentary rock. like a salt pan in a desert. not possible to have volcanic rocks originate this way.

crystalization in molten earth: slow cooling over time. (hundreds to millions of years)

crystalization at earth's surface: this results in fast cooling. (a few hours to a few months or years)

crystalization from cooling off hot water: that would be a hydrothermal deposit. while associated with volcanics they are not volcanic rocks themselves and usually occur fairly rapidly.