A long elastic body of aerodynamically bluff cross-section, capable of exhibiting either galloping or vortex-induced transverse vibrations in a flow normal to its length, can, if lightly damped, also exhibit large-amplitude vibrations related to the two above forms, but not predictable from information available for either form considered separately. Before a rational explanation of this behaviour can be given it is necessary to have some detailed experimental evidence of the exciting forces on the body during these vibrations. To this end the authors have made wind tunnel measurements on a freely-oscillating cylinder of square section under closely two-dimensional conditions in both smooth and turbulent flow. The test cylinder was constrained to one degree of freedom by air bearings in an elastic system mounted on a rigid external frame independent of the wind tunnel structure. Linear springs and variable magnetic system damping were used. The aerodynamic excitation was measured using a pressure manifold connected to pressure taps along a streamwise line on one face of the test model at mid-span, and reporting to a transducer. Two key theoretical parameters are dimensionless wind speeds, Urfor system resonance with the wake vortex street, and U0for the initiation of galloping. With the highest damping U0was well above Ur and for all turbulence levels the measurements of both excitation and response supported the predictions of galloping theory. With the lowest system damping U0 was less than r for all turbulence levels, and in these cases oscillation always began at Urand cylinder amplitude increased monotonically with U, while the fluctuating pressure excitation was dominated by the component synchronized with the body motion, except near U=3Ur where a peak of the same order occurred in the component at three times body frequency, with corresponding kinks in the body amplitude curves. Generally, the spectrum of the excitation was found to depend strongly on the ratio U0/Ur. All of the parameters appearing in theoretical models of vortex-induced and galloping oscillations were measured in the experiments, and the observed phenomena are analysed in the light of existing knowledge of the two basic forms of oscillation and of existing and possible theoretical models.