Colloidal shear thickening presents a significant challenge because the macroscopic rheology becomes increasingly controlled by the microscopic details of short ranged particle interactions in the shear thickening regime. Our measurements here of the first normal stress difference over a wide range of particle volume fraction elucidate the relative contributions from hydrodynamic lubrication and frictional contact forces, which have been debated. At moderate volume fractions we find N1 < 0, consistent with hydrodynamic models, however at higher volume fractions and shear stresses these models break down and we instead observe dilation (N1 > 0), indicating frictional contact networks. Remarkably, there is no signature of this transition in the viscosity, instead this change in the sign of N1 occurs while the shear thickening remains continuous. These results suggest a scenario where shear thickening is driven primarily by the formation of frictional contacts, with hydrodynamic forces playing a supporting role at lower concentrations. Motivated by this picture, we introduce a simple model which combines these frictional and hydrodynamic contributions and accurately fits the measured viscosity over a wide range of particle volume fraction and shear stress. [3] suggesting that contact friction plays a dominant role in colloidal shear thickening, however this assertion is controversial because of contrary evidence. While friction-based models and simulations capture the viscosity increase observed in experiments, other experimental signatures, particularly the stress anisotropy, are at odds with expectations for frictional interactions [4].Shear thickening, where a suspension's viscosity η = σ/γ increases with increasing shear stress σ (or shear rateγ), is important in a wide array of industrial processes and applications, either something to be avoided or a desired, engineered property [5][6][7]. Shear thickening is observed in both granular suspensions, where the particle diameter d is generally d 10 µm, and colloidal suspensions, where d 10 µm. In granular suspensions, the evidence that friction drives shear thickening is well established [8][9][10][11][12][13][14][15][16] but in colloidal suspensions shear thickening is instead commonly attributed to diverging hydrodynamic lubrication forces, which lock particles together in correlated 'hydroclusters' [17][18][19][20][21].A key difference between friction and lubrication forces lies in the stress anisotropy generated by these two types of interactions. This difference is captured by the first normal stress difference N 1 ≡ σ xx − σ zz , where σ ij is the stress tensor for a shear flow in the x direction with a gradient along z. Simulations based on hydrodynamic interactions show that shear-induced distortions of the suspension microstructure and short ranged lubrication forces drive N 1 < 0 [7,18,19,22]. Including repulsive interactions or elastic particle deformations to these hydrodynamic models does not change the sign of N 1 [23][24][25], and N 1 is predicte...