The so-called stripe phase of the manganites is an important example of the complex behaviour of metal oxides, and has long been interpreted as the localisation of charge at atomic sites 1,2,3,4 . Here, we demonstrate via resistance measurements on La 0.50 Ca 0.50 MnO 3 that this state is in fact a prototypical charge density wave (CDW) which undergoes collective transport. Dramatic resistance hysteresis effects and broadband noise properties are observed, both of which are typical of sliding CDW systems. Moreover, the high levels of disorder typical of manganites result in behaviour similar to that of well-known disordered CDW materials. Our discovery that the manganite superstructure is a CDW shows that unusual transport and structural properties do not require exotic physics, but can emerge when a well-understood phase (the CDW) coexists with disorder.The stripe phase in manganites of the form La 1−x Ca x MnO 3 appears as the temperature is lowered through T ≃ 240 K, and the superstructure wavevector settles on a final value of q≃ (1 − x)a * 1 (where a * is the reciprocal lattice vector) for 0.5 ≤ x < 0.85, at T ≃ 120 K 2 . Based on the insulating nature of the manganites up to room temperature, and the observation of stripes of charge order in transmission electron microscopy (TEM) images, early studies concluded that the superstructure arose from localisation of charge at atomic sites 3,4 . However, neutron and xray studies found the degree of charge localisation at Mn sites to be small, and subsequent theoretical work suggested that a CDW model may be more applicable 5 . This suggestion is supported by the observation that q/a * is strongly temperature dependent 2,6 , indicating that a model in which the superstructure periodicity is derived from the sample stoichiometry cannot be valid. In addition, heat capacity peaks at the transition to the stripe phase can be modelled as "dirty Peierls transitions", expected in a disordered CDW system 7 . However, the possibility of the stripe phase exhibiting sliding behaviour, as seen in many other CDW systems 8 , could not be probed without the ability to make orientation-dependent resistivity measurements. Here we describe the first such measurements on the manganite stripe phase, which reveal dramatic