Recognizing the errors of route surveys, Brigade-Major William Lambton proposed a grand scientific project in 1800: to measure the curvature of the Earth and construct a mathematical gridiron of triangles across India. On 10 April 1802, the GTS commenced with a 7.5-mile baseline measurement at St. Thomas Mount, Madras, using the colossal 36-inch Ramsden Theodolite (weighing 1,016 lbs).
When Lambton died in 1823, his brilliant assistant Col. Sir George Everest took command (Surveyor General 1830–1843). Everest introduced the invar-like Colby Compensation Bars to eradicate thermal distortion and devised the "Gridiron System" spanning north-south and east-west across India. Everest computed the Everest 1830 Spheroid ($a = 6,377,276.345\text{ m}, 1/f = 300.8017$), which remains the foundational geodetic datum for the subcontinent.
In 1852, Indian mathematical prodigy and Chief Computer Radhanath Sickdhar computed the trigonometric zenith calculations from Dehradun, discovering that Peak XV was the highest mountain in the world at 29,002 ft (8,848 m). In 1856, Surveyor General Andrew Waugh named it Mount Everest in honor of his predecessor.
- The Great Arc: Spanned 2,400 km from Cape Comorin (8°N) to Banog near Mussoorie (30°N)—the longest and most accurate meridional arc measured on Earth at the time.
- Tower Construction: In flat regions like Bengal, hundreds of 60-foot masonry towers were constructed through jungle and malaria zones to clear line-of-sight for theodolites.