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Used by Heller for model ships. 1:250 scale is commonly used with aircraft models - usually rather large and fairly pricey models - such as jumbo jet scale models. [7] 1:239: 1.275 mm Used by some model aircraft. 1:220: 1.385 mm: Model railways (Z) Same as Z gauge. 1:200: 0.06 in: 1.524 mm: Architecture. Ship models. Die-cast aircraft
The 1:200 scale is a modeling scale used in the model building hobby. A vehicle or building made in the 1:200 scale, fits 200 times inside its real-life counterpart (in one dimension; it would fit 8 million times if packed three-dimensionally, and would weigh 8 million times less).
The Fuller calculator, sometimes called Fuller's cylindrical slide rule, is a cylindrical slide rule with a helical main scale taking 50 turns around the cylinder. This creates an instrument of considerable precision – it is equivalent to a traditional slide rule 25.40 metres (1,000 inches) long.
The scale can be expressed in four ways: in words (a lexical scale), as a ratio, as a fraction and as a graphical (bar) scale. Thus on an architect's drawing one might read 'one centimeter to one meter', 1:100, 1/100, or 1 / 100 . A bar scale would also normally appear on the drawing.
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Following the patent and release of Harold's Long Scale calculator featuring two knobs on the outside rim in 1914, he designed the Magnum Long Scale calculator in 1927. [6] [7] As the name "Magnum" implies, it was a fairly large device at 4.5 inches in diameter—about 1.5 inches more than Fowler's average non-Magnum-series calculators. [8]
One scale foot is equivalent to approximately 12/200 of an inch, 0.06 inches and 1.524 millimetres. One scale yard is equivalent to approximately 1/36 of an inch, 0.18 inches and 4.572 millimetres. Figure scale is 8 mm generally squared off to 1/190 – 1/220 scale. 10 mm: ≈1.667 mm - ≈1.9 mm: ≈1:182 - 1:160
Each iteration of the Sierpinski triangle contains triangles related to the next iteration by a scale factor of 1/2. In affine geometry, uniform scaling (or isotropic scaling [1]) is a linear transformation that enlarges (increases) or shrinks (diminishes) objects by a scale factor that is the same in all directions (isotropically).