How is true north commonly determined?

True north is commonly determined by geographical mapping from the Earth's surface. This approach involves using the geographic coordinates of locations mapped out based on the Earth's rotation and its position in relation to celestial bodies. The North Pole represents true north, and understanding the Earth's geography allows for accurate representation of this direction on maps.

Mapping techniques take into account the curvature of the Earth and the relationship between latitude and longitude, enabling navigators and geographers to establish a reference point for true north. While other methods might provide approximations or different concepts of north, such as magnetic north influenced by a compass or grid north used in specific mapping systems, geographic mapping remains the fundamental method for determining true north based on the Earth's orientation in space.