Equidistant
In geometry, equidistant refers to the relationship between points, lines, or figures that maintain an equal distance from one another or from a specified reference point.[1] This concept is fundamental, describing scenarios where the separation between elements is identical, such as two points being the same distance from a third point or parallel lines remaining constantly apart.[2][3] The principle of equidistance plays a central role in defining key geometric structures and theorems. For instance, all points on a circle are equidistant from its center, forming the basis for circular geometry and properties like radii and circumferences.[4] Similarly, the perpendicular bisector of a line segment consists of all points equidistant from its two endpoints, which is essential for constructions and proofs involving symmetry.[5] In coordinate geometry, the locus of points equidistant from two fixed points is the perpendicular bisector line, a concept applied in solving systems of equations and analyzing distances via the distance formula.[6] Equidistant relationships extend to broader applications in mathematics and related fields, underpinning Euclidean constructions where tools like compasses identify sets of equidistant points to create regular polygons and divide segments accurately.[7] This idea also informs real-world uses, such as in navigation for locating positions midway between landmarks or in engineering for ensuring balanced designs in structures like bridges and antennas.[8] Overall, equidistance ensures precision in spatial reasoning, making it a cornerstone of geometric analysis.[9]Definition and Fundamentals
General Definition
Equidistant describes the property in which two or more points, lines, or objects maintain equal distances from a given reference point or from one another.[3][2] This concept is fundamental in geometry, where it identifies relationships based solely on distance equality without regard to angles or other measures. For instance, every point on the circumference of a circle is equidistant from its center, defining the circle's boundary as the locus of such points.[10][11] The term originates from Late Latin aequidistantem, formed by combining aequi- ("equal") and distantem ("distant" or "standing apart"), entering English via French in the late 16th century.[12][13] Its earliest recorded mathematical use appears in 1570, in a translation by Henry Billingsley, reflecting the growing formalization of geometric ideas among European scholars during the Renaissance.[13] Equidistant differs from "isometric," which pertains to transformations or mappings that preserve all distances between points, such as rotations or reflections in Euclidean space.[14] It also contrasts with "congruent," a term for geometric figures that match exactly in shape and size, achievable through isometric transformations like translations or flips.[15][16]Mathematical Formulation
In Euclidean geometry, the distance between two points P = (x_1, y_1) and Q = (x_2, y_2) in the plane is given by the formula d(P, Q) = \sqrt{(x_2 - x_1)^2 + (y_2 - y_1)^2}, which derives from the Pythagorean theorem applied to the right triangle formed by the points and their projections on the axes.[17] A point P is equidistant from two fixed points A and B if d(P, A) = d(P, B).[18] This condition generalizes to n-dimensional Euclidean space, where points are represented as vectors \mathbf{P}, \mathbf{A}, \mathbf{B} \in \mathbb{R}^n, and the distance is the Euclidean norm \|\mathbf{P} - \mathbf{A}\| = \|\mathbf{P} - \mathbf{B}\|, with \|\mathbf{v}\| = \sqrt{\sum_{i=1}^n v_i^2} for a vector \mathbf{v}.[17] Equivalently, squaring both sides yields \|\mathbf{P} - \mathbf{A}\|^2 = \|\mathbf{P} - \mathbf{B}\|^2, which simplifies to the linear equation $2(\mathbf{B} - \mathbf{A}) \cdot \mathbf{P} = \|\mathbf{B}\|^2 - \|\mathbf{A}\|^2.[18] The set of all points P satisfying d(P, A) = d(P, B) forms the perpendicular bisector of the segment AB. In two dimensions, this is a line passing through the midpoint of AB and perpendicular to it; in three dimensions, it is a plane.[18] To derive the equation of this locus in the plane, consider fixed points A = (a_1, a_2) and B = (b_1, b_2), and a variable point P = (x, y). The equidistance condition is \sqrt{(x - a_1)^2 + (y - a_2)^2} = \sqrt{(x - b_1)^2 + (y - b_2)^2}. Squaring both sides eliminates the square roots: (x - a_1)^2 + (y - a_2)^2 = (x - b_1)^2 + (y - b_2)^2. Expanding yields x^2 - 2a_1 x + a_1^2 + y^2 - 2a_2 y + a_2^2 = x^2 - 2b_1 x + b_1^2 + y^2 - 2b_2 y + b_2^2. Canceling x^2 and y^2 from both sides simplifies to -2a_1 x + a_1^2 - 2a_2 y + a_2^2 = -2b_1 x + b_1^2 - 2b_2 y + b_2^2, or rearranging terms, $2(b_1 - a_1)x + 2(b_2 - a_2)y = b_1^2 + b_2^2 - a_1^2 - a_2^2. This is the Cartesian equation of a straight line, confirming the locus as the perpendicular bisector.[19]Applications in Geometry
Basic Properties and Examples
In geometry, a fundamental property of a circle is that it consists of all points in a plane equidistant from a fixed central point, with this constant distance known as the radius. This equidistance ensures that every point on the circumference maintains the same separation from the center, defining the circle's shape and symmetry.[20] Another key property in a circle involves chords: two congruent chords are equidistant from the center, meaning their midpoints lie at the same distance from the center along perpendicular lines from the center to the chords. The line segment from the center to the midpoint of any chord is perpendicular to that chord, and for equal chords, the midpoints share this equidistant positioning, highlighting the circle's radial uniformity.[20] A classic example of equidistant points arises in triangles, where the circumcenter is the point equidistant from all three vertices, serving as the center of the circumcircle that passes through those vertices. This center can lie inside an acute triangle, on the hypotenuse of a right triangle, or outside an obtuse triangle, but it always maintains equal distances to the vertices, enabling the construction of the circumcircle.[21] Equidistant configurations in polygons often imply symmetry, particularly in regular polygons where all vertices are equidistant from the center, resulting in rotational symmetry of order equal to the number of sides and multiple axes of reflectional symmetry passing through the center and vertices or side midpoints. This central equidistance underscores the balanced structure of such polygons, distinguishing them from irregular forms.[22] To demonstrate how equal distances lead to isosceles triangles, consider a proof sketch using triangle congruence: suppose in triangle ABC, sides AB and AC are equal in length (AB = AC). Let M be the midpoint of base BC, so BM = MC. The triangles ABM and ACM share side AM and have AB = AC and BM = MC, making them congruent by SSS (side-side-side). Consequently, the base angles at B and C are equal (∠ABC = ∠ACB), confirming the triangle is isosceles with AB and AC as the equal sides. This congruence approach similarly applies via SAS when an included angle is considered.[23]Loci and Conic Sections
In geometry, the locus of points equidistant from a fixed point, known as the center, forms a circle. This definition captures the essential property that every point on the circle lies at a constant distance, the radius, from the center, distinguishing it as a closed curve in the plane.[24] A parabola arises as the locus of points equidistant from a fixed point, called the focus, and a fixed line, termed the directrix. This equidistance condition ensures that for any point on the parabola, the perpendicular distance to the directrix equals the distance to the focus, producing the characteristic U-shaped curve. The standard equation for a parabola with vertex at (h, k), opening upward or downward, is given by (x - h)^2 = 4p (y - k), where p is the distance from the vertex to the focus (or directrix), and the sign of p determines the direction of opening./05:_Conic_Sections__Circle_and_Parabola/5.02:_The_Equation_of_the_Parabola)/07:_Hooked_on_Conics/7.03:_Parabolas) In contrast, ellipses and hyperbolas, while related as conic sections, do not satisfy a strict equidistant condition but instead involve constant sums or differences of distances to two fixed points, the foci. An ellipse is the locus where the sum of distances to the foci is constant, with eccentricity e < 1, while a hyperbola is the locus where the absolute difference of distances to the foci is constant, with e > 1. These definitions highlight the unique role of equidistance in circles (where e = 0, effectively one focus coinciding with the center) and parabolas (e = 1), emphasizing balanced distance measures over additive or subtractive ones./09:_Curves_in_the_Plane/9.01:_Conic_Sections)[25] The locus of points equidistant from two intersecting lines consists of the pair of angle bisectors formed by those lines. This property arises because the perpendicular distance from any point on the bisector to each line is equal, providing a fundamental construction in plane geometry for dividing angles symmetrically.[26] The theoretical foundations of conic sections, including loci defined by distance properties like equidistance, were advanced by Apollonius of Perga in the 3rd century BCE through his systematic treatment of these curves as plane figures.[27]Applications in Cartography
Equidistant Projections
Equidistant projections in cartography are map projections designed to preserve true distances from one or two specific points or along particular lines, thereby minimizing distortion in those directions while allowing variation elsewhere.[28] These projections are neither conformal nor equal-area, but they provide a useful compromise for applications where accurate measurement from a central reference is prioritized over shape or area preservation.[28] By maintaining scale along radials or standard lines, they facilitate distance calculations in navigation and regional mapping.[28] The azimuthal equidistant projection exemplifies this approach, centering the map on a single point—typically a pole in the polar aspect or along the equator in the equatorial aspect—from which distances to all other points are preserved radially.[28] In the polar version, meridians appear as straight lines radiating from the center, while parallels form concentric circles with spacing proportional to latitude; the equatorial version features a straight central meridian and equator, with the outer meridian as a semicircle.[28] The mathematical basis derives from spherical trigonometry, where the radial distance \rho from the origin to a point is given by \rho = [R](/page/R) \theta, with [R](/page/R) as the Earth's radius and \theta (or c) as the angular distance in radians from the center.[28] Coordinates are then computed as x = \rho \sin \theta and y = -\rho \cos \theta, where \theta is the difference in longitude from the central meridian.[28] Another key variant is the equidistant conic projection, which projects the globe onto a cone tangent or secant at one or two standard parallels, preserving true scale along those parallels and along all meridians.[28] Meridians radiate as straight lines from an apex beyond the pole, spaced equally, while parallels appear as arcs of concentric circles with constant spacing.[28] This makes it particularly suitable for mid-latitude regions spanning east-west, such as parts of North America or Europe, where distortion remains moderate between the standard parallels.[28] The projection's simplicity arises from its reliance on basic conic geometry, with forward formulas involving the distance p along a meridian as p = R (\cot \beta_0 - \cot \beta), where \beta relates to latitude and \beta_0 to the standard parallel.[28] The development of equidistant projections traces back to antiquity, with the azimuthal equidistant known for over 2,000 years and used by ancient Egyptians for star charts; its application to Earth maps emerged in the 16th century for navigation, notably for the polar insets in Gerardus Mercator's 1569 world map.[28] The equidistant conic originated in rudimentary form with Ptolemy in the 2nd century AD and saw refinement during the Renaissance for regional charts.[28] These projections gained prominence in modern cartography through their adoption in official surveys, such as U.S. Geological Survey maps of polar regions and mid-latitude areas.[28]Properties and Specific Types
Equidistant projections preserve distances accurately along specific lines or from designated points, making them valuable for applications requiring precise measurement in those directions. In cylindrical equidistant projections, such as the Plate Carrée, distances along all meridians and along the equator are maintained true, with parallels represented as equally spaced horizontal lines.[29] The azimuthal equidistant variant, centered on a pole or other point, ensures that distances and directions from the center to any other point on the globe are correct, while shapes remain undistorted near the center but become increasingly elliptical toward the edges.[30] This property arises from projecting the globe onto a plane tangent at the center, preserving radial distances without scaling distortion from that origin.[29] Despite these strengths, equidistant projections introduce significant distortions in areas and angles away from the standard lines or central point. Areas tend to expand or contract unevenly, particularly in higher latitudes, and angles are not preserved, leading to shape deformations that increase with distance from the reference lines.[31] For global representations, especially in polar-centered azimuthal versions, the opposite hemisphere suffers extreme exaggeration, rendering the projection unsuitable for comprehensive world maps where balanced portrayal is needed.[29] These limitations stem from the inherent trade-offs in flattening the spherical surface, where prioritizing distance preservation sacrifices other geometric properties.[30] Among specific types, the two-point equidistant projection extends the distance-preserving quality to two designated foci, maintaining true scale along all lines radiating from either point to any other location on the map. This makes it particularly useful for regional mapping where accurate distances between two key centers—such as major cities or seismic stations—are essential. The sinusoidal projection, a pseudocylindrical variant, functions as a pseudo-equidistant map by spacing parallels equally and preserving areas exactly, though it curves meridians sinusoidally to achieve equal-area without true equidistance along all meridians.[32] It balances distance approximation along the equator with area fidelity, ideal for thematic world maps emphasizing continental extents.[29] Practical examples highlight these projections' utility in targeted scenarios. The azimuthal equidistant projection forms the basis of the United Nations emblem, depicting the world as viewed from the North Pole with continents arranged around the pole in a circle of constant latitude, emphasizing global unity through accurate polar distances.[33] It is also employed for Antarctic mapping by the U.S. Geological Survey, where the projection's polar centering allows precise distance measurements across the continent from the South Pole, supporting scientific and navigational efforts in the region.[34] To illustrate distortions relative to other common projections, the following table compares key properties of azimuthal equidistant and Mercator projections:| Property | Azimuthal Equidistant | Mercator |
|---|---|---|
| Distance Preservation | True from center point; distorted elsewhere | True only along the equator; distorted elsewhere, increasingly toward the poles |
| Area Preservation | Distorted, with expansion away from center | Severely distorted, enlarging high latitudes |
| Angle Preservation | Not preserved; shapes deform at edges | Preserved (conformal); maintains local shapes |
| Suitability | Polar/regional maps requiring radial distances | Navigation charts needing constant bearings |