Cercocarpus montanus var. glaber (S. Wats.) F. L. Martin

rocky canyon northwest below Emory Peak, in volcanic rhyolite gravels. Note: leaves large and glabrous, also the distinctive long curved styles arising from achenes are mostly bare, not plumose as is normal

rocky canyon northwest below Emory Peak, in volcanic rhyolite gravels. Note: leaves large and glabrous (with age), also the distinctive long curved styles arising from achenes are mostly bare, not plumose as is normal

rocky canyon northwest below Emory Peak, in volcanic rhyolite gravels. Note: leaves large and glabrous (with age), also the distinctive long curved styles arising from achenes are mostly bare, not plumose as is normal

rocky canyon northwest below Emory Peak, in volcanic rhyolite gravels. Note: leaves large and glabrous (with age), also the distinctive long curved styles arising from achenes are mostly bare, not plumose as is normal

rocky canyon northwest below Emory Peak, in volcanic rhyolite gravels. Note: leaves large and essentially glabrous (with age) rising from substantial woody base.