GELE Geodesy — Figure of the Earth and the Reference EllipsoidConcept Map
If you learn better by seeing ideas connected visually, this concept map of Figure of the Earth and the Reference Ellipsoid is built for you. Every GELE Geodesy question draws on these relationships, so building this map mentally is half the battle when you sit for GELE 2026.
Exam context
On the GELE 2026, the Geodesy subtest carries a "Core" weight in Professional Regulation Commission (PRC) — Board of Geodetic Engineering's pattern. Figure of the Earth and the Reference Ellipsoid lands at position 1st out of 6 in the standard review order. Target score is 70% weighted average, no sub-test below 50%, and roughly a meaningful share of items come from Geodesy on a typical GELE paper.
Figure of the Earth and the Reference Ellipsoid - Concept Map
Central Concept
Reference Ellipsoid as the Mathematical Model of Earth's Shape
Related Concepts
Concept
Earth's Physical Shape
Sub Concepts
- Oblate spheroid geometry
- Flattening at the poles
- Equatorial bulge
- Actual Earth surface (geoid)
Relationship To Central
Real-world phenomenon that the reference ellipsoid models and approximates
Concept
Ellipsoid Definition Parameters
Sub Concepts
- Semi-major axis (a) — equatorial radius
- Semi-minor axis (b) — polar radius
- Flattening (f)
- First eccentricity squared (e²)
- Second eccentricity squared (e'²)
Relationship To Central
Mathematical quantities that completely define a reference ellipsoid
Concept
Parameter Relationships
Sub Concepts
- f = (a − b)/a
- b = a(1 − f)
- e² = 2f − f²
- e² = (a² − b²)/a²
- e'² = (a² − b²)/b²
Relationship To Central
Algebraic interconnections between ellipsoid definition parameters
Concept
Radii of Curvature
Sub Concepts
- Prime vertical radius (N) — east–west curvature
- Meridian radius (M) — north–south curvature
- Mean radius of curvature (R) — Gaussian mean
- Latitude-dependent variations
- Applications in distance/area calculations
Relationship To Central
Measures of how the ellipsoid curves at any point, varying with latitude
Concept
Global Reference Systems
Sub Concepts
- WGS84 — GNSS and global standard
- PRS92 — Philippine Reference System
- Clarke 1866 — historical reference
- GRS80 — Geodetic Reference System 1980
- Ellipsoid selection criteria
Relationship To Central
International ellipsoid standards adopted for positioning and mapping
Concept
Geodetic Applications
Sub Concepts
- Coordinate system establishment
- Geodetic datum definition
- Mapping projections (UTM, PPCS)
- Distance and area reductions
- Height systems and vertical datum
Relationship To Central
Practical uses of ellipsoid parameters in surveying and mapping work
Concept
Philippine Geodetic Context
Sub Concepts
- RA 4374 — Subdivision of Land for Sale
- RA 8560 — Property Boundary Markers
- PD 1529 — Creation of Cadastral Maps
- CA 141 — Public Land Act provisions
- PRS92 mandatory adoption
Relationship To Central
Regulatory and practical application frameworks specific to Philippine surveying
Concept Connections
To
Semi-minor axis (b)
From
Semi-major axis (a)
Strength
strong
Relationship
b is calculated from a and flattening f using the formula b = a(1 − f)
To
First eccentricity squared (e²)
From
Flattening (f)
Strength
strong
Relationship
e² is derived from f using e² = 2f − f²; the two parameters both characterize ellipsoid shape
To
Prime vertical radius (N)
From
First eccentricity squared (e²)
Strength
strong
Relationship
e² appears in the denominator of N = a/√(1 − e²sin²φ); controls curvature variation with latitude
To
Meridian radius (M)
From
First eccentricity squared (e²)
Strength
strong
Relationship
e² appears in both numerator and denominator of M = a(1−e²)/(1−e²sin²φ)^1.5; controls north–south curvature
To
Meridian radius (M)
From
Prime vertical radius (N)
Strength
strong
Relationship
Both vary with latitude φ; N ≥ M everywhere; combined as mean radius R = √(MN) for local sphere approximations
To
Prime vertical radius (N)
From
Latitude φ
Strength
strong
Relationship
N varies continuously with latitude; equals a at equator (φ=0°) and equals pole value at poles (φ=90°)
To
Meridian radius (M)
From
Latitude φ
Strength
strong
Relationship
M varies continuously with latitude; equals a(1−e²) at equator and approaches a at poles
To
PRS92 — Philippine Reference System
From
WGS84 — GNSS and global standard
Strength
strong
Relationship
PRS92 is adopted for official Philippine surveying; WGS84 is the GNSS ellipsoid; coordinate transformations between them are necessary
To
Geodetic datum
From
Reference Ellipsoid
Strength
strong
Relationship
The ellipsoid is the surface on which a geodetic datum is established by defining an origin point and orientation
To
Coordinate system establishment
From
Ellipsoid parameters (a, b, f, e²)
Strength
strong
Relationship
Ellipsoid parameters define the geometric foundation upon which latitude–longitude coordinates and their associated radii of curvature are calculated
To
Distance and area reductions
From
Radii of curvature (N, M, R)
Strength
strong
Relationship
N and M are used to reduce geodetic distances and areas to the ellipsoid and further to map projections (UTM, PPCS)
To
Reference ellipsoid
From
Mapping projections (UTM, PPCS)
Strength
strong
Relationship
Both UTM and PPCS are mathematically defined transformations from the ellipsoid surface to a plane; they depend on ellipsoid parameters and radii of curvature
To
PRS92 — Philippine Reference System
From
RA 4374 — Subdivision of Land for Sale
Strength
strong
Relationship
RA 4374 mandates the use of PRS92 ellipsoid and datum for all cadastral subdivision surveys in the Philippines
To
PRS92 — Philippine Reference System
From
RA 8560 — Property Boundary Markers
Strength
moderate
Relationship
Boundary markers must reference the PRS92 coordinate system as established by RA 4374
To
Reference Ellipsoid
From
PD 1529 — Creation of Cadastral Maps
Strength
strong
Relationship
Cadastral maps must be constructed using the official reference ellipsoid (PRS92) and datum for legal recognition
To
Equatorial bulge
From
Oblate spheroid geometry
Strength
strong
Relationship
The equatorial bulge is the physical manifestation of Earth's oblate shape; a > b causes this bulge
To
Reference Ellipsoid
From
Actual geoid surface
Strength
moderate
Relationship
The ellipsoid is a mathematical model that approximates the geoid; the geoid is Earth's true equipotential surface
To
Second eccentricity squared (e'²)
From
Flattening (f)
Strength
moderate
Relationship
e'² = (a² − b²)/b² is an alternative shape parameter related to f through the ellipsoid axes
To
GNSS Positioning
From
WGS84 — GNSS and global standard
Strength
strong
Relationship
WGS84 is the fundamental ellipsoid and datum upon which all GNSS positioning (GPS, GLONASS, Galileo) is based
To
Historical reference
From
Clarke 1866
Strength
moderate
Relationship
Clarke 1866 is a historical ellipsoid used in older surveys and some coordinate systems; understanding it aids in datum transformation and legacy data interpretation
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