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Below are two tables which report the average adult human height by country or geographical region. With regard to the first table , original studies and sources should be consulted for details on methodology and the exact populations measured, surveyed, or considered.
Height measurement using a stadiometer. Human height or stature is the distance from the bottom of the feet to the top of the head in a human body, standing erect.It is measured using a stadiometer, [1] in centimetres when using the metric system or SI system, [2] [3] or feet and inches when using United States customary units or the imperial system.
The tallest U.S. president was Abraham Lincoln at 6 feet 4 inches (193 centimeters), while the shortest was James Madison at 5 feet 4 inches (163 centimeters). Donald Trump , the current president, is 6 feet 3 inches (190 centimeters) according to a physical examination summary from February 2019.
In statistics, a standard normal table, also called the unit normal table or Z table, [1] is a mathematical table for the values of ...
Height 160 cm 5 ft 3 in Waist 72 cm 28 in ... Normal weight obesity – Metabolically obese normal weight; ... Toggle the table of contents.
The normal seat height for a bar stool is 30" (76 cm) with a 26" (66 cm) stool being used against kitchen counters. Extra tall 36" (91 cm) stools are increasingly used in contemporary styles with high pub tables to create a visual effect in modern interiors. Counter height bar stools have a seat height of 24" (61cm).
A billiard table or billiards table is a bounded table on which cue sports are played. In the modern era, all billiards tables (whether for carom billiards , pool , pyramid or snooker ) provide a flat surface usually made of quarried slate , that is covered with cloth (usually of a tightly woven worsted wool called baize ), and surrounded by ...
Normal heights (symbol or ; SI unit metre, m) is a type of height above sea level introduced by the Soviet scientist Mikhail Molodenskii.The normal height of a point is defined as the quotient of a point's geopotential number C (i.e. its geopotential difference with that of sea level), by the vertically averaged normal gravity: