An analysis is presented of the maximum thickness of a stationary buoy
ant oil-mass, trapped under an angled incline, when subjected to hydro
dynamic, surface tension and buoyancy forces. For high water-flow spee
ds down the aquifer, with upward buoyancy forces dominantly combating
hydrodynamic pressure, it is shown that the maximum oil thickness occu
rs at about 60% of the length of the oil stringer measured from the up
ward end. The length of the oil stringer then is roughly proportional
to the square root of the oil-mass contained, as is the maximum thickn
ess. For low water-flow speeds, in which buoyancy and surface tension
are dominantly balanced (with only lesser contributions from hydrodyna
mic pressure), the oil length is effectively constant, whereas the max
imum thickness grows proportionately to the 3/4 power of the contained
oil mass at low oil masses, and proportionately to the oil mass at hi
gh mass values. As the water-flow velocity increases, the shaping of t
he oil stringer shifts from the small ''bubble'' form to the long oil
stringer form. Analytic formulae are given to provide approximate meth
ods from which to estimate oil and gas accumulations under more comple
x conditions.