The Riemann curvature tensor R^ρ_{σμν} is the mathematical object that encodes the intrinsic curvature of spacetime — the genuine gravitational field that cannot be eliminated by any coordinate choice. It measures the failure of parallel transport to commute around closed loops, and equivalently the relative acceleration of nearby geodesics (tidal forces, via the geodesic deviation equation). It is constructed from the Christoffel symbols and their first derivatives: R^ρ_{σμν} = ∂_μ Γ^ρ_{νσ} - ∂_ν Γ^ρ_{μσ} + Γ^ρ_{μλ}Γ^λ_{νσ} - Γ^ρ_{νλ}Γ^λ_{μσ}. In four dimensions the Riemann tensor has 20 independent components (reduced from 256 by its symmetries), which fully characterize the curvature at each point. All other curvature quantities — the Ricci tensor, Ricci scalar, Weyl tensor, and Einstein tensor — are derived from it.
The Christoffel symbols tell you how basis vectors change from point to point, but they are coordinate-dependent — they can be made to vanish at any single point. The Riemann curvature tensor, by contrast, is a true tensor that cannot be eliminated by any coordinate choice. It captures the intrinsic curvature of spacetime, the genuine gravitational content that exists independently of how you label events. If R^ρ_{σμν} = 0 everywhere, spacetime is flat and gravity is absent (though coordinate effects may mimic it). If R^ρ_{σμν} ≠ 0, spacetime is genuinely curved and no coordinate system can make it look flat.
The most intuitive definition of the Riemann tensor comes from parallel transport. Take a vector and parallel-transport it around a small closed loop in spacetime. In flat space, the vector returns to its original orientation. In curved spacetime, it comes back rotated. The Riemann tensor measures this rotation: for a small loop spanning the μ-ν plane, the change in a vector V^ρ after transport around the loop is proportional to R^ρ_{σμν} V^σ times the area of the loop. This is the path-dependence of parallel transport, and it is the defining characteristic of curvature. The same phenomenon appears on a curved two-dimensional surface: parallel-transport a vector around a triangle on a sphere and it returns rotated by an angle proportional to the enclosed area and the Gaussian curvature.
Physically, the Riemann tensor manifests as tidal forces through the geodesic deviation equation. Consider two nearby freely falling particles with four-velocity u^μ and infinitesimal separation vector ξ^μ. Their relative acceleration is D²ξ^μ/dτ² = -R^μ_{νρσ} u^ν ξ^ρ u^σ. This equation is the GR equivalent of the Newtonian tidal force equation (where tidal acceleration is proportional to the gradient of the gravitational field). Near any massive body, the Riemann tensor produces stretching along the radial direction and compression in the transverse directions — the tidal deformations that would eventually "spaghettify" an object falling into a black hole. Gravitational wave detectors like LIGO work by sensing the oscillating tidal forces described by this equation.
The Riemann tensor in four dimensions has 256 nominal components (R^ρ_{σμν} with each index running from 0 to 3), but its algebraic symmetries reduce the independent components to 20. These symmetries include antisymmetry in the first and second pairs of indices (when fully lowered), symmetry under exchange of the two pairs, and the algebraic Bianchi identity (vanishing of the cyclic sum over three indices). Additionally, the differential Bianchi identity ∇_{[λ} R_{ρσ]μν} = 0 provides further constraints that are crucial for the consistency of the Einstein field equations. The 20 independent components decompose into the 10 components of the Ricci tensor R_{μν} (which Einstein's equations relate directly to matter) and the 10 components of the Weyl tensor C_{ρσμν} (the trace-free part, representing the "free" gravitational field that propagates in vacuum as gravitational waves).