Using electron spin resonance spectroscopy (ESR), we measure the rotational mobility of probe molecules highly diluted in deeply supercooled bulk water and negligibly constrained by the possible ice fraction. The mobility increases above the putative glass transition temperature of water, T g ؍ 136 K, and smoothly connects to the thermodynamically stable region by traversing the so called ''no man's land'' (the range 150 -235 K), where it is believed that the homogeneous nucleation of ice suppresses the liquid water. Two coexisting fractions of the probe molecules are evidenced. The 2 fractions exhibit different mobility and fragility; the slower one is thermally activated (low fragility) and is larger at low temperatures below a fragile-to-strong dynamic cross-over at Ϸ225 K. The reorientation of the probe molecules decouples from the viscosity below decoupling of transport properties ͉ dynamic cross-over in water ͉ dynamic heterogeneity ͉ supercooled water ͉ polycrystalline materials T he physical properties of water are far from being completely understood. Several thermodynamic and dynamic anomalies are known or anticipated in the metastable supercooled regime that influence the equilibrium states and have deep impact in biology, astrophysics, glaciology, and atmospheric science (1-3). At ambient pressure, the supercooled regime ranges between the commonly accepted value of the glass transition temperature T g ϭ 136 K and the freezing temperature T m ϭ 273.15 K. Above T g , amorphous water transforms into a highly viscous fluid (4, 5). Crystallization into metastable cubic ice (I c ) at T X Ϸ 150 K with further transformation to the usual hexagonal form of ice I h is reported (1, 6). On the other hand, bulk water at atmospheric pressure can be supercooled below its melting temperature down to the homogeneous nucleation temperature T H Ϸ 235 K, below which it usually crystallizes to I h . Thus, the region between T X and T H is often regarded as a region where liquid water cannot be observed [''no man's land,'' NML (1)]. Nonetheless, the coexistence of crystals and deeply supercooled liquids was suspected almost 1 century ago for bulk systems (7). More recently, evidence that water and cubic ice coexist in thin films in the temperature range 140-210 K was reported (8-11). The existence of liquid water has been also shown experimentally in veins (or so-called triple junctions) of polycrystalline ice (12) that serve as interfacial reservoirs for impurities (13-15). The size of such reservoirs is thermodynamically defined by surface forces and also by the curvature of the surface (i.e., the Kelvin effect in veins) (11, 16). In pure ice, the reservoir size increases when approaching the melting point (17). Notably, recent simulations concluded that in polycrystalline materials grain boundaries exhibit the dynamics of glass-forming liquids (45).This background motivated us to investigate the coexistence of ice and supercooled water in large volumes in an attempt to characterize the dynamical properties of the li...