Coordinate geometry, also known as analytic geometry, is the study of geometric figures using a coordinate system in which points are represented by numerical coordinates. It provides a powerful bridge between algebra and geometry, allowing geometric shapes to be described by equations and algebraic operations to yield geometric insights. Key concepts include plotting points, finding distances, midpoints, slopes, and the equations of lines, circles, and conic sections on the Cartesian plane.
| Concept | Formula | Variables | Example |
|---|---|---|---|
| Distance between two points | d = √((x₂−x₁)² + (y₂−y₁)²) | x₁,y₁,x₂,y₂ = coordinates | (1,2)→(4,6): d=5 |
| Midpoint of a segment | M = ((x₁+x₂)/2, (y₁+y₂)/2) | Endpoints (x₁,y₁),(x₂,y₂) | (2,4)&(6,8): M=(4,6) |
| Slope of a line | m = (y₂−y₁)/(x₂−x₁) | m = slope | (1,1)&(3,5): m=2 |
| Equation of a line | y = mx + c | m = slope, c = y-intercept | y = 3x + 2 |
| Equation of a circle | (x−a)² + (y−b)² = r² | (a,b) = centre, r = radius | centre(2,3), r=5 |
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The midpoint formula gives the coordinates of the point that lies exactly halfway between two given points on a line segment in the Cartesian plane. It is derived by averaging the x-coordinates and the y-coordinates of the two endpoints separately. The midpoint is used extensively in geometry proofs, construction of perpendicular bisectors, and in applications such as GPS interpolation and computer graphics.
The distance formula gives the straight-line (Euclidean) distance between two points in the Cartesian plane using their coordinates. It is derived directly from the Pythagorean theorem by treating the horizontal and vertical separations as legs of a right triangle. The formula extends naturally to three dimensions as d = √((x₂−x₁)² + (y₂−y₁)² + (z₂−z₁)²) and is fundamental in analytic geometry, physics, and data science.
A conic section is a curve obtained by intersecting a right circular cone with a plane at various angles, yielding four distinct types: circle, ellipse, parabola, and hyperbola. These curves were first studied systematically by the Greek mathematician Apollonius of Perga (c. 262–190 BCE) and later became fundamental in physics when Kepler showed that planetary orbits are ellipses. Conic sections are described by the general second-degree equation Ax² + Bxy + Cy² + Dx + Ey + F = 0, and the type is determined by the discriminant B² − 4AC.
The word "coordinate" comes from Latin "co-" (together) + "ordinare" (to arrange in order). The system was independently developed by René Descartes and Pierre de Fermat in the 17th century; Descartes' 1637 work "La Géométrie" is the foundational text. The field is sometimes called "Cartesian geometry" in his honour.