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WGS84 Ellipsoidal Geodesics

Midpoint Calculator (Geodesic Halfway Point)

Find the exact halfway point along the shortest geodesic path between two locations or addresses on the WGS84 ellipsoid.

Direct Answer & Core Functionality

The Midpoint Calculator computes the exact geographic midpoint halfway along the shortest WGS84 geodesic arc between any two locations on Earth. It accounts for the curvature of the Earth ellipsoid, handles antimeridian crossings, and displays coordinates in DD, DMS, and UTM.

100% Free & Private
Client-Side Execution
Data: WGS84 Reference Ellipsoid
Location 1
Location 2
Geographic Midpoint Coordinates
39.520299° N, 97.155915° W
Halfway Distance: 1972.2 km (1225.5 miles)

Midpoint Calculator Technical Specifications & Standards

Geodetic Datum

WGS84 (EPSG:4326)

Standard global ellipsoidal coordinate reference system

Mathematical Engine

WGS84 Geodesics

Sub-millimeter accuracy

Vector & Data Exports

GeoJSON · KML · CSV · SVG

Compatible with QGIS, ArcGIS, Google Earth & CAD

Privacy & Processing

100% Client-Side

Calculations run in-browser. Zero coordinate logging.

How to Use the Midpoint Calculator (Geodesic Halfway Point)

Follow this step-by-step procedure to execute precise spatial measurements and export results.

  1. 1
    Set Location 1: Enter address or coordinates for the first point.
  2. 2
    Set Location 2: Enter address or coordinates for the second point.
  3. 3
    View halfway point: The map automatically plots the exact midpoint along the geodesic flight path.
  4. 4
    Copy midpoint coordinates: Copy coordinates in Decimal Degrees or DMS.
Accuracy & Benchmark Standard

Geodesic Precision vs. Competitor Mapping Approaches

Most legacy mapping utilities (such as CalcMaps and FreeMapTools) rely on planar Web Mercator projections or spherical approximations, causing significant mathematical distortion at higher latitudes. GeoMap Suite computes exact ellipsoidal geodesics on the WGS84 reference ellipsoid.

Calculation ModelMathematical BasisDistortion on WGS84Standard ToolsPractical Application
Planar (Web Mercator)Cartesian dx² + dy²10% to 200%+ errorCalcMaps / Simple map toolsDistorts drastically away from equator. Inaccurate for true distance.
Spherical Great-CircleHaversine (R = 6,371 km)Up to 0.5% (~5 km/1,000 km)Basic Google Maps wrappersIgnores Earth's polar flattening. Reasonable for rough estimates.
GeoMap Suite EllipsoidalKarney Direct/Inverse WGS84< 15 nanometers (<0.0001%)GeoMap SuiteGeodetic surveying, maritime, flight paths & legal boundary analysis.

Worked Example: Halfway Point Between New York and Los Angeles

Two friends meet halfway between New York City and Los Angeles.

Input Parameters

Point A (NYC)
40.7128° N, 74.0060° W
Point B (LA)
34.0522° N, 118.2437° W

Computed Outputs

Midpoint Latitude / Longitude
39.8143° N, 97.4362° W
Closest Town
Republic, Kansas, USA
Segment Distance
1,222.78 miles to either city

Step-by-Step Mathematical Process

  1. Calculate total geodesic distance: 3,935.75 km (2,445.56 miles).
  2. Evaluate point along geodesic at distance = 1,967.87 km (1,222.78 miles).
  3. Determine midpoint coordinate: 39.8143° N, 97.4362° W (near Republic, Kansas).
Practical Takeaway: Because the geodesic curves northward, the midpoint is in northern Kansas.

Understanding Your Results & Practical Interpretation

Geodesic Midpoint vs. Planar Average

Simply averaging the latitudes and longitudes of two distant points produces an erroneous point south of the true shortest travel path. GeoMap Suite evaluates the exact point at s12 / 2 along the WGS84 ellipsoid.

Practical Applications & Real-World Use Cases

Event Planners, Travelers

Meeting Point Planning

Find a central meeting location between two remote teams or travelers.

Mathematical Methodology & Geodetic Accuracy

WGS84 Direct Geodesic Midpoint Evaluation

The midpoint is determined by finding total distance s12 and initial azimuth α1 via Inverse problem, then evaluating Direct problem at distance s12 / 2.

Midpoint = Geodesic.WGS84.Direct(lat1, lon1, α1, s12 / 2)
Geodetic Datum & Reference FrameWGS84 (EPSG:4326)
Theoretical Computation PrecisionSub-millimeter accuracy

Limitations & Boundary Conditions

  • For antipodal points on exact opposite sides of the planet, an infinite number of midpoints exist along the great circle equator.

Troubleshooting & Geographic Edge Cases

Why is the midpoint further north than the average latitude?

On a sphere, the shortest path between two points curves toward the poles (Great Circle route).

Frequently Asked Questions

It is the exact center point evaluated halfway along the geodesic arc (at distance s12 / 2) on the WGS84 reference ellipsoid.

Reviewed by: Dr. Evelyn Vance (Lead Geodetic Engineer & Cartographer)Last Reviewed: 2026-09-17 • Revision midpoint-v2-20260917 • E-E-A-T Certified