TOOLS · CROSS-SECTION · TEXAS

2 wells, subsea datum

West to east, 0.4 miles end to end. Subsea datum.

How to read it →

Each column is a well, lettered in the order drawn: west to east when every well has a location, or the order you list them (drag a well in the list, or switch to "As listed"). A well with no tops filed is listed but not drawn.

Under the subsea datum depths are elevation minus measured depth, so tops line up regardless of surface terrain; a value above zero sits above sea level. When not every well reports an elevation the section is in measured depth and the columns are not datum-aligned.

Each formation filed in more than one well has its own color, joined between neighboring wells and shaded down to the next formation both filed. Nothing is interpolated.

Where tops come from →

Section · 2 wells drawn

0-500-1,000-1,500SUBSEA FTA1,125 FT ELB1,103 FT ELSaddle CreekSaddle Creek

shaded: a formation down to the next one filed in both wellsfiled in one well onlypoint at or tap a top to read it

Tops by well

Subsea feet, with measured depth beneath; the name as filed where it differs; a dash where the well has no top filed for the formation.

  • AWaggoner Dntw #2623DN
  • BWaggoner Dntk #243DN
FormationAB
Coleman Junction288 MD 837COLEMAN JUNCTION - CORROSIVE ZON—
Dothan Lime—56 MD 1,047
Tannehill—-84 MD 1,187TANNEHILL SAND
Saddle Creek-307 MD 1,432-277 MD 1,380
Dyson—-696 MD 1,799
Breckenridge Lime—-758 MD 1,861
Megargel Lime—-881 MD 1,984
Gunsight—-1,064 MD 2,167GUNSIGHT SAND
Milham—-1,289 MD 2,392
Canyon-1,732 MD 2,857CANYON REEF—

About this data

Formation tops and elevations from the RRC dbf900 wellbore file (completion filings), names normalized to the formations registry; well identity from the permit record, location from the shared well record. Subsea is elevation minus measured depth. Nothing between filed tops is estimated.

New to these records? completion reports and the wellbore file

Developers: this page as JSON is GET /v1/data/cross-section, documented in the API reference.