Lateral variations in point bar deposits Cross-section perpendicular to flow: BIotcTbateu, dessicalIcnFsrackec mud Seals:alc crsc sfialiRed sand Chia'IIEI il dEposi.s ) Gare- scale cross stialifitsa2so-s Note basal erosion surface and lag deposit. Also note bedding geometry in bar deposit: lateral accretion beds dipping tonight, formed from lateral accretion on point bar ithin lateral accretion beds, paleocurrents are directed out of the outcrop, if the outcrop is oriented perp endicular to flow Channel fill deposits consist of fining upward sediments in beds conformable with channel, formed by vertical accretionLateral variations in point bar deposits