TOOLS · CROSS-SECTION · TEXAS

2 wells, subsea datum

West to east, 0.3 miles end to end. Depths are elevation minus measured depth, so tops line up regardless of surface terrain; a value above zero sits above sea level. 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 →

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2,000-0-2,000-4,000-6,000-8,000SUBSEA FTA3,328 FT ELB3,320 FT ELDelawareDelaware

shaded: a formation down to the next one filed in both wellsfiled in one well onlyhover a top or a name to pick out one formation

Tops by well

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

FormationAMesquite State UnitBCopperhead
Rustler—2,378MD 942
Salado—2,068MD 1,252
Bell Canyon162MD 3,166—
Delaware162MD 3,166159MD 3,161
Cherry Canyon-805MD 4,133—
Brushy Canyon-1,864MD 5,192—
Bone Spring-2,967MD 6,295—
Wolfcamp-5,296MD 8,624—
Atoka-9,511MD 12,839—

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Only wells with a location on file can be found by distance; a well with tops but no location can still be added by name or API number.

The tops, as filed

Apache Corporation · Culberson · 3,328 ft elevation · 16,000 ft TD

FormationMD ftSubsea
Delaware3,166162
Bell Canyon3,166162
Cherry Canyon4,133-805
Brushy Canyon5,192-1,864
Bone SpringBONE SPRINGS6,295-2,967
Wolfcamp8,624-5,296
Atoka12,839-9,511

BCopperhead #901 42-109-33271

Apache Corporation · Culberson · 3,320 ft elevation · 5,000 ft TD

FormationMD ftSubsea
Rustler9422,378
Salado1,2522,068
Delaware3,161159

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.