Example 1
- l = 2
- N = 50000
- unit = cm
100,000 cm = 1 km
What is 2 cm at 1:50,000? 1 km.
Enter map length l and scale denominator N from the 1:N notation. Ground length in the same unit is L = l × N. At 2 cm and 1:50,000 the result is 100,000 cm = 1 km. At 5 cm and 1:25,000 it is 125,000 cm = 1.25 km. The calculator does not compute area scale N² or the reverse conversion from ground to map.
Enter l > 0 and N > 0.
Domain: l > 0 and N > 0. Map and ground units match for the product; the cm/mm/m/in list drives conversions. This is not the rule of three with an unknown, and not areal scale N².
Map scale written 1:N (the representative fraction, RF) means one unit of length on the map equals N units of the same measure on the ground. When you enter map length l and denominator N, ground length in that same unit is L = l × N. With l = 2 cm and N = 50,000 the result is 100,000 cm, or 1 km. With l = 3 cm and N = 1,000 the result is 3,000 cm (30 m). With l = 1.5 cm and N = 2,000 the result is 3,000 cm (30 m).
The mathematical model is the linear representative fraction, the school-cartography standard: RF = 1/N = l/L, hence L = l × N. Ordnance Survey and map-reading manuals stress that both lengths must share a unit before multiplying; only then do you convert cm to m or km. This calculator shows L in the map unit and also as metres, kilometres, and miles.
The calculator uses the numbers you enter in fields l (skala-mapy-dlugosc-a) and N (skala-mapy-dlugosc-b). The domain is l > 0 and N > 0. Zero or a negative value returns an error. The unit list (cm, mm, m, in) does not change the formula — it only converts the result. Comma and period are equivalent.
The result panel shows L, echoes of l and N, the RF 1:N label, and conversions. The bar diagram compares map and ground segments schematically (not true metre scale). The calculator does not apply a projection scale factor k and does not compute areal scale N². The rule of three solves a different unknown in a proportion; here N is already known.
Worked examples: 2 cm and 50,000 → 100,000 cm = 1 km; 3 cm and 1,000 → 3,000 cm; 1.5 cm and 2,000 → 3,000 cm; 5 cm and 25,000 → 125,000 cm = 1.25 km; 1 in and 63,360 → 1 mile; 4 cm and 100,000 → 400,000 cm = 4 km. l = 0 or N = 0 returns an error.
L = l × N for l > 0, N > 0.
RF = 1/N = l/L (representative fraction).
Conversion: Lm = L · u, where u is metres per map unit (cm → 0.01; mm → 0.001; m → 1; in → 0.0254).
Symbols: l — map length (skala-mapy-dlugosc-a); N — denominator of 1:N (skala-mapy-dlugosc-b); L — ground length. Mathematical model: linear representative fraction (RF).
Numeric map scale 1:N is the representative fraction (RF). The numerator is always 1 (the map segment), and denominator N states how many times longer the matching ground segment is when both lengths use the same unit. If l is map length and L is ground length, then RF = l/L = 1/N, so the calculator formula is L = l × N.
RF is dimensionless: 1 cm on a 1:50,000 map equals 50,000 cm on the ground, and 1 mm equals 50,000 mm. Changing the unit does not change N; it only changes how you rewrite L before converting to kilometres. This calculator requires N > 0 and l > 0, because RF does not describe a zero or negative segment.
In teaching practice it helps to separate the mathematical product from measurement error: a paper ruler gives l to about a millimetre, while ground distance may come from GPS or a tape. The calculator returns the exact product of the numbers you enter (floating-point arithmetic), not field survey error.
Ratio scales are older than digital cartography. Medieval and early modern maps often used verbal scales (“an inch to a mile”) and graphic scale bars. The representative fraction spread with military topography and national mapping agencies: it compares maps across languages because it does not depend on inches versus metres.
Ordnance Survey (UK) and USGS (United States) teach RF as the basis for reading distance: measure l, multiply by N, convert units. The International Cartographic Association (ICA) treats scale as a core legend element. ISO 19111 covers reference systems and projections where a local scale factor k can differ from the sheet’s nominal RF — this calculator does not apply that k.
Conceptually one distinguishes linear scale (lengths), areal scale (areas, roughly N² under local isotropy), and verbal scale. Over large regions a projection makes a single RF true only locally or along a standard parallel. This educational model stays with pure L = l × N.
For l > 0, N > 0: L = l · N, RF = 1/N = l/L. The map (l, N) ↦ L is bilinear on the positive domain. Inverses: l = L/N and N = L/l when L and l are known and positive.
Homogeneity: if you rescale l and L by the same unit factor (cm → mm ×10), N is unchanged. Areal scale under local isotropy is about 1:N², but that is not this page’s result.
Comparing scales: larger N means a smaller-scale map in cartographic English (less detail per ground area). A 1:10,000 map is larger-scale than 1:100,000 — more detail for the same ground extent.
In teaching practice it helps to separate the mathematical formula from floating-point limits: this calculator shows the browser’s floating-point product. When N is extreme, check the domain first, then floating-point arithmetic range.
Step 1. RF definition: one map unit equals N ground units, so the map-to-ground length ratio is 1/N.
Step 2. For a map segment of length l: L / l = N / 1 because the ratio is constant. Hence L = l · N.
Step 3. Unit conversion: let u be metres per one map unit (cm → 0.01 m, in → 0.0254 m). Then L_m = (l · N) · u. Kilometres: L_km = L_m / 1000. Miles: L_mi = L_m / 1609.344.
Step 4 (example). l = 2 cm, N = 50,000 → L = 100,000 cm. L_m = 100,000 · 0.01 = 1,000 m = 1 km. That matches the classic 1:50,000 topo-map reading.
Step 5 (inverse). If you know L and l in matching units, N = L/l. This calculator does not solve for unknown N — it takes N as given; the rule of three or a two-number ratio serve other setups.
School PL example: 2 cm on a 1:50,000 map → 1 km on the ground. US classic: 1 in on a 1:63,360 map → 1 statute mile (63,360 in = 1 mi). With N = 1,000 and l = 3 cm → 30 m. With N = 25,000 and l = 5 cm → 1.25 km. With N = 100,000 and l = 4 cm → 4 km.
N = 1 means a 1:1 model. N approaching zero is rejected (error). Very large N (atlas maps) yields huge L even for small l — expected, while the on-screen bars stay schematic only.
In teaching practice it helps to separate the formula from field measurement limits: GPS and tape have their own error, which this calculator does not model.
The calculator computes a plain floating-point arithmetic product l * N. Comma and period in the fields are equivalent. Integer results format without useless decimals; fractions keep several significant digits in the panel.
Choosing cm/mm/m/in only affects the L label and the m/km/mi conversions. The calculator does not load a map file or measure screen pixels — you enter l by hand.
With an extremely large N the product may leave the floating-point arithmetic range; then an error message appears instead of infinity in the result.
Related: rule of three (proportion with an unknown), ratio of two numbers, distance between two points (coordinates, not map scale). Areal scale and projection factor k are separate models.
Sources: Wikipedia — Scale (map); Ordnance Survey — Guide to cartography: Scale; USGS / map-reading manuals on representative fraction; ISO 19111 (reference systems; context for k). Educational tool — not a substitute for a geodetic survey.
L = l × N at scale 1:N. 2 cm and 50,000 give 100,000 cm = 1 km.
100,000 cm = 1 km
What is 2 cm at 1:50,000? 1 km.
3,000 cm = 30 m
What is 3 cm at 1:1,000? 30 m.
3000 cm
What is 1.5 cm at 1:2,000? 30 m.
125,000 cm = 1.25 km
What is 5 cm at 1:25,000? 1.25 km.
error
What if l = 0? Outside the domain.
error
What if N = 0? Outside the domain.
63,360 in = 1 mi
What is 1 in at 1:63,360? 1 mile.
400,000 cm = 4 km
What is 4 cm at 1:100,000? 4 km.
It converts ground length L from map length l at numeric scale 1:N. The formula is L = l × N in matching units. With l = 2 cm and N = 50,000 the result is 100,000 cm, which is 1 km.
It is the representative fraction (RF): one unit on the map equals N units of the same measure on the ground. N is the scale denominator. You enter N alone — you do not enter the leading “1 :”.
L = 2 × 50,000 = 100,000 cm. That is 1,000 m = 1 km. It is the first worked example on this page and the same result after “Fill this example”.
3 × 1,000 = 3,000 cm (30 m). 1.5 × 2,000 = 3,000 cm (30 m). Both use the same L = l × N formula.
Both must satisfy l > 0 and N > 0. Zero or a negative map length or scale denominator returns an error, because RF 1:N does not describe a map segment then.
Yes for the core product: centimetres on the map times N yield centimetres on the ground. The unit list (cm, mm, m, in) only drives helper conversions to metres, kilometres, and miles — it does not change L = l × N.
The rule of three solves a/b = c/x. Here you already know scale 1:N and multiply map length by N. It is the same ratio expressed as an RF denominator, without a fourth unknown.
No. The model is pure linear RF. A projection scale factor k (for example in UTM) is not applied. Areal scale N² is not computed either.
1 × 63,360 = 63,360 inches on the ground, which is exactly one statute mile. That is the classic inch-to-mile school example.
Yes. 1.5 and 1,5 are the same length. With N = 2,000 the result is 3,000 in the map unit.
No. The result depends on l, N, and the map-unit choice in the form. The currency and unit settings in the page header do not affect this result.
An empty l or empty N leaves the result blank. The calculator does not insert a default scale when a value is missing.
Multiply the map length by the scale denominator: L = l × N. With 2 cm and 1:50,000: 2 × 50,000 = 100,000 cm = 1 km. Enter l and N (without “1 :”).
4 × 25,000 = 100,000 cm = 1 km. Same arithmetic as 2 cm on 1:50,000 — the result depends on the product l × N.
No. The fields take l and N, and the result is L = l × N. The reverse l = L / N is not a separate mode on this page.
No. The result is horizontal length from a linear scale. A curved path and elevation gain make the on-foot distance longer than this model.
A smaller denominator N means a larger (more detailed) scale. For the same map length l, 1:25,000 gives a ground distance four times shorter than 1:100,000.
The RF definition and L = l × N below come from recognized cartographic sources.
Page updated November 3, 2026.