We report on the simultaneous Giant Metrewave Radio Telescope (GMRT) and Algonquin Radio Observatory (ARO) observations at 550-750 MHz of the scintillation of PSR B1508+55, resulting in a ∼10,000-km baseline. This regime of measurement lies between the shorter few 100-1000 km baselines of earlier multi-station observations and the much longer earth-space baselines. We measure a scintillation cross-correlation coefficient of 0.22, offset from zero time lag due to a ∼ 45 s traversal time of the scintillation pattern. The scintillation time of 135 s is 3× longer, ruling out anisotropic as well as strictly 1D scattering. Hence, the low cross-correlation coefficient is indicative of highly anisotropic but 2D scattering. The common scintillation detected on the baseline is confined to low delays of 1𝜇s, suggesting that this correlation may not be associated with the prominent parabola detected at GMRT. Detection of pulsed echoes and their direct imaging with the Low Frequency Array (LOFAR) by a different group enable them to measure a distance of 120 pc to the screen causing these echoes. These previous measurements, alongside our observations, lead us to propose that there are two scattering screens: the closer 120 pc screen causing the prominent parabola detected at GMRT, and a screen further beyond causing the scintillation detected on the GMRT-ARO baseline. We advance the hypothesis that the 120-pc screen partially resolves the speckle images on the screen beyond and that their scattering axes are mutually misaligned, resulting in a two-dimensional scattered disc, to explain the low cross-correlation coefficient.