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The AAPG/Datapages Combined Publications Database

GCAGS Transactions


Gulf Coast Association of Geological Societies Transactions
Vol. 41 (1991), Pages 432-441

Sedimentology of a modern point bar at raven camp on the Red River, central Louisiana

Brian E. Lock (1), Catherine E. Bishop (1)


The Red River Waterway is a Congressionally-funded project designed to establish a navigation channel from the Mississippi River to Shreveport. Channel straightening in the Raven Camp area, at River Mile 136, has artificially cut off a meander loop and lowered local base level, so that the point bar is almost completely exposed at low water stage in the late summer and fall, while winter and spring high waters still completely submerge the bar and reactivate sediment transport. Air photographs taken over the past twenty years record a surprising rate of channel migration and shifting sites of sand accumulation; these processes continue today, despite artificial constraints by the U. S. Army Corps of Engineers.

As the spring flood waters recede, they expose a variety of sedimentary structures, dominated by sand Previous HitwavesNext Hit over most of the bar surface. At the downstream end of the bar, where floodwaters rejoin the navigation channel, the sand Previous HitwavesNext Hit have heights of up to two feet, although over most of the bar they average six inches; the crest to crest interval is between ten and fifteen feet. Climbing linguoid ripples cover the uneroded surfaces of the sand Previous HitwavesNext Hit, and grade up to mud drapes which mark the last stages of individual floods. Large scale foreset bedding characterizes the bar margin adjacent to the low water channel, and well developed reactivation surfaces are common.

During the stage of receding waters, symmetrical wave ripples having a wave length (crest to crest) of slightly more than one inch are formed by wind-generated Previous HitwavesTop in very shallow standing water close to the water's edge. Dropping water stages are recorded by convolute lamination and by internally chaotic beds of fluidized sand. These are structures that relate to dewatering of the sediment. Desiccation cracks and curled-up mudflakes are common. Many mud clasts are incorporated in subsequent flood-stage sands. After exposure, point bar sands are further modified by raindrop impacts and associated erosion and by the formation of rills and deep gullies during storm water run-off. During dry weather periods, eolian transport begins and texturally distinctive ripples form. Adhesion structures develop on damp sands close to the water's edge during eolian episodes.

Biological traces are surprisingly common, and include the effects of rooted plants (particularly from the fast growing willow seedlings), vertebrate and insect traces, algal mats, and associated biogenic gas escape structures. Deposits of one winter/spring season are commonly scoured and removed the following year, followed by fresh deposition over a different part of the bar. Scour surfaces are abundant internal features of the point bar.

Study of the Raven Camp point bar over a period of several years provides important lessons for the explorationist seeking hydrocarbon s in fluvial sands. Many of the sedimentary structures that might be seen in conventional cores are not ones traditionally regarded as indicative of point bar sands, and the reservoir heterogeneity and facies architecture are far more complex than much of the literature would suggest.

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