Abstract
In these proceedings, we discuss recent results from d+Au collisions in PHENIX ridge related measurements and their possible hydrodynamic origin. We present the v2 at midrapidity and measurements of the pseudorapidity dependence of the ridge, distinguishing between the d-going and Au-going directions. We investigate the possible geometrical origin by comparing v2 in d+Au to that in p+Pb, Au+Au and Pb+Pb collisions. Future plans to clarify the role of geometry in small collision systems at RHIC are discussed.
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