We compute the flux of relic neutrino background (RB) up-scattered by ultra-high-energy (UHE) cosmic rays (CRs) in clusters that act as CR-reservoirs. The long trapping times of UHECRs make this flux larger than that of RB up-scattered by UHECRs on their way to Earth, which we also compute. We find that IceCube excludes RB weighted overdensities larger than in clusters, and that PUEO, RNO-G, GRAND and IceCube-Gen2 will test values down to . Our treatment incorporates the momentum transfer dependence of the neutrino-nucleus cross section, deep inelastic scattering, a mixed UHECR composition, and flavour information on the up-scattered RB fluxes for both cases of neutrino mass spectrum with normal and inverted ordering, providing new handles to possibly disentangle the up-scattered RB from cosmogenic neutrinos.

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