The Glenmora plate. Relief from Copernicus GLO-30; rivers and lakes from USGS NHD; watersheds from the USGS Watershed Boundary Dataset; roads and city limits from Census TIGER 2024.
Mostly sunny
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Showers likely
Mostly sunny; warmer
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Glenmora’s center stands about 140 ft above sea level. Within three miles the land runs from 90 ft to 210 ft, a difference of 120 ft: gently rolling country.
Under the town center the state geologic map shows Intermediate Terraces (clay, silt), from the Pleistocene, less than 2.6 million years old.
The section below crosses 4 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 64×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Clay, silt. Age: Pleistocene, less than 2.6 million years old. About 11 mi of the line.
Clay, silt, sand. Age: Pleistocene, less than 2.6 million years old. About 9 mi of the line.
Clay. Age: Holocene, less than 12,000 years old. About 4 mi of the line.
Clay, silt, sand. Age: Pleistocene, less than 2.6 million years old. About 0.4 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale.
Heights from Copernicus GLO-90 (a surface model: it includes buildings and tree canopy); summits from USGS GNIS; rivers from USGS NHDPlus HR; rock from the USGS State Geologic Map Compilation.
A raindrop that lands in Glenmora reaches the Gulf of America by way of Little Spring Creek, the Bayou Cocodrie, the Bayou Boeuf, the Bayou Teche and the Lower Atchafalaya: about 230 river miles.
140 miles of the trip are on the Bayou Teche.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Glenmora; river miles along the main stem, rounded.
