We investigate both experimentally and numerically the impact of liquid drops on deep pools of aqueous glycerol solutions with variable pool viscosity and air pressure. With this approach we are able to address drop impacts on substrates that continuously transition from low-viscosity liquids to almost solids. We show that the generic corolla spreading out from the impact point consists of two distinct sheets, namely an ejecta sheet fed by the drop liquid and a second sheet fed by the substrate liquid, which evolve on separated timescales. These two sheets contribute to a varying extent to the corolla overall dynamics and splashing, depending in particular on the viscosity ratio between the two liquids.Throwing a stone in a stagnant pond or letting a waterdrop fall onto a dry plate equally contribute to the active pleasures of water splashing [1], as does the rewarding observation of the short-lived liquid corolla which, in both cases, blooms on the impact point [2]. From a comprehensive point of view however, the dynamics of the two events remarkably differif only for the matter-of-fact reason that the splashed liquid belongs to the projectile in the latter, and to the impacted substrate in the former. The case of a liquid drop hitting a liquid surface therefore raises a natural question: which of the two liquids feeds the corolla as it spreads out, develops and eventually disintegrates? How does the splashing dynamics relate to that of the two first problems? Splashes are formally defined as the ejection of small droplets due to the large deformation of a liquid interface following an impact, and occur in a large diversity of problems related to challenging environmental and industrial applications [3][4][5][6][7][8][9]. In particular, two manifestations of splashing are discussed at length in the literature, referred to as 'prompt splash' [10][11][12] and 'crown splash' [12,13], and mostly discriminated by the dynamics, shape and behaviour of the liquid sheet (which we will generically refer to as corolla) whose desintegration results in the ejection of droplets. Prompt splash is associated with the early destabilisation of a thin ejecta sheet shooting out almost horizontally from the impact point: this axisymmetric liquid jet expands radially, bends upwards and disintegrates into small and fast droplets [10,12,14,15]. On the other hand, crown splash originates in the destabilisation of an almost vertically expanding liquid sheet (sometimes referred to as Peregrine sheet [12]) rising out of the impact region [1,12,16]. Here the 'crown' emerges through the fingering of the liquid rim at the leading edge of the Peregrine sheet, owing to coupled Rayleigh-Taylor (RT) and Rayleigh-Plateau (RP) instabilities, and produces somewhat larger droplets [12,[16][17][18]. However, some considerable confusion remains regarding the precise characterisation of these two splashing regimes and associated corolla dynamics. Indeed, the complicated splashing phenomenology rarely allows for such a clear separation between the coroll...