“…These and other authors (Servio and Englezos, 2003;Ohmura et al, 2004) examined hydrate crust mor phologies: a more faceted aspect (individual crystals of millimeter sizes) is observed at low subcooling ΔT, while a smooth appearance is noted at intermediate and high ΔT. Extensive observations of hydrate crust texture and lateral growth at water/gas interfaces have been conducted over the past decade, most of them focused on water/CH 4 systems, using various configurations: a rising (gas) bubble in water (Peng et al, 2007;Sun et al, 2007;Li et al, 2013Li et al, , 2014, a water drop (in gas) either pendent (Zhong et al, 2011) or sitting on a substrate (Tanaka et al, 2009), or a planar water/gas interface (Kitamura and Mori, 2013). While there is some scatter in the published lateral growth rates, all observations show that the hydrate crust texture gets smoother with increasing subcooling and increasing time.…”