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An initially-stationary object which is allowed to fall freely under gravity drops a distance which is proportional to the square of the elapsed time. Height = gravity constant * time^2. Time = 3.5 s. Gravity constant = 9.8m/s/s. 9.8 * 3.5^2 = 120.05

### Semantic Tags:

**gravity constant**
The **gravitational constant**, approximately 6.67×10−11 N·(m/kg)2 and denoted by letter *G*, is an empirical physical constant involved in the calculation(s) of gravitational force between two bodies. It usually appears in Sir Isaac Newton's law of universal gravitation, and in Albert Einstein's theory of general relativity. It is also known as the **universal gravitational constant**, **Newton's constant**, and colloquially as **Big G**. It should not be confused with "little g" (*g*), which is the local gravitational field (equivalent to the free-fall acceleration), especially that at the Earth's surface.

**Celestial mechanics**
**Celestial mechanics** is the branch of astronomy that deals with the motions of celestial objects. The field applies principles of physics, historically classical mechanics, to astronomical objects such as stars and planets to produce ephemeris data. Orbital mechanics (astrodynamics) is a subfield which focuses on the orbits of artificial satellites. Lunar theory is another subfield focusing on the orbit of the Moon.

**Introductory physics**
The following outline is provided as an overview of and topical guide to physics:

**Physics** – natural science that involves the study of matter and its motion through spacetime, along with related concepts such as energy and force. More broadly, it is the general analysis of nature, conducted in order to understand how the universe behaves.

**Obsolete scientific theories**
A **superseded**, or **obsolete, scientific theory** is a scientific theory that mainstream scientific consensus once commonly accepted but now no longer considers the most complete description of reality, or simply false. This label does not cover protoscientific or fringe science theories with limited support in the scientific community. Also, it does not mean theories that were never widely accepted. Some theories that were only supported under specific political authorities, such as Lysenkoism, may also be described as obsolete or superseded.

In some cases a theory or idea is found baseless and is simply discarded. For example, the phlogiston theory was entirely replaced by the quite different concept of energy and related laws. In other cases an existing theory is replaced by a new theory that retains significant elements of the earlier theory; in these cases, the older theory is often still useful for many purposes, and may be more easily understood than the complete theory and lead to simpler calculations. An example of this is the use of Newtonian physics, which differs from the currently accepted relativistic physics by a factor that is negligibly small at velocities much lower than that of light. All of Newtonian physics is so satisfactory for most purposes that it is more widely used except at velocities not small compared with that of light, and simpler Newtonian but not relativistic mechanics is usually taught in schools. Another case is the theory that the earth is approximately flat; while it has for centuries been known to be wrong for long distances, considering part of the earth's surface as flat is usually sufficient for many maps covering areas that are not extremely large, and surveying.

**Gravity of Earth**
The **gravity of Earth**, denoted **g**, refers to the acceleration that the Earth imparts to objects on or near its surface. In SI units this acceleration is measured in meters per second squared (in symbols, m/s2 or m·s−2) or equivalently in newtons per kilogram (N/kg or N·kg−1). It has an approximate value of 9.81 m/s2, which means that, ignoring the effects of air resistance, the speed of an object falling freely near the Earth's surface will increase by about 9.81 metres (32.2 ft) per second every second. This quantity is sometimes referred to informally as *little g* (in contrast, the gravitational constant *G* is referred to as *big G*).

There is a direct relationship between gravitational acceleration and the downwards weight force experienced by objects on Earth, given by the equation *ma* = *F* (*force* = *mass* × *acceleration*). However, other factors such as the rotation of the Earth also contribute to the net acceleration.

**Le Sage's theory of gravitation**
**Le Sage's theory of gravitation** is a kinetic theory of gravity originally proposed by Nicolas Fatio de Duillier in 1690 and later by Georges-Louis Le Sage in 1748. The theory proposed a mechanical explanation for Newton's gravitational force in terms of streams of tiny unseen particles (which Le Sage called ultra-mundane corpuscles) impacting all material objects from all directions. According to this model, any two material bodies partially shield each other from the impinging corpuscles, resulting in a net imbalance in the pressure exerted by the impact of corpuscles on the bodies, tending to drive the bodies together. This mechanical explanation for gravity never gained widespread acceptance, although it continued to be studied occasionally by physicists until the beginning of the 20th century, by which time it was generally considered to be conclusively discredited.

**Equations for a falling body**
A set of **dynamical equations** describe the resultant trajectories when objects move owing to a constant gravitational force under normal Earth-bound conditions. For example, Newton's law of universal gravitation simplifies to *F* = *mg*, where m is the mass of the body. This assumption is reasonable for objects falling to earth over the relatively short vertical distances of our everyday experience, but is very much untrue over larger distances, such as spacecraft trajectories. Please note that in this article any resistance from air (drag) is neglected.

**Physics**
**Gravitation**
**Gravimetry**