Summary — Aspects of the water relations of three oak species (Quercus gambelii, Q turbinella and Q macrocarpa) and their hybrids (Q gambelii x turbinella, Q gambelii x macrocarpa) were observed under common garden conditions in northern Utah, USA. In the absence of summer moisture inputs, Q macrocarpa and Q turbinella were unable to maintain active gas exchange through the day; following an early morning peak, leaf conductances to water vapor remained very low through the remainder of the day. In contrast, Q gambelii and the hybrids were able to maintain high leaf conductances throughout this period. Consistent with these observations, Q gambelii is thought to have a root system penetrating to the deeper, winter-recharged layers, a feature apparently absent in both Q macrocarpa or Q turbinella. Based on current hybrid distributions, both Q turbinella and Q macrocarpa once extended into drier more northerly regions than they occupy at present. When these parents retreated, they left behind hybrids with Q gambelii, which do not depend on monsoonal moisture input. Leaf size, leaf longevity, carbon isotope ratio, and minimum winter temperatures appear not to be correlated with the absence of Q macrocarpa and Q turbinella from summer-dry habitats. Instead it appears that reliance on summer monsoon events is one of the critical factors influencing loss of these oaks from summer-dry sites in the intermountain west.