TOOLS · CROSS-SECTION · TEXAS

2 wells, subsea datum

West to east, 3.8 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 →

AE B King #12 tops×BYarbrough #215 tops×
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500-0-500-1,000-1,500-2,000SUBSEA FTA958 FT ELB1,299 FT ELTrinity Water Sands - H…Trinity Water Sands - High Wash-CiscoCisco

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.

FormationAE B KingBYarbrough
Trinity Water Sands - High Wash-658MD 300949MD 350
Cisco-672MD 1,630-1,007MD 2,306
Canyon—-1,753MD 3,052
Strawn—-1,863MD 3,162
Brazos River—-2,177MD 3,476

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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

AE B King #1 42-337-00151

Tettleton, Steven B. · Montague · 958 ft elevation · 1,850 ft TD

FormationMD ftSubsea
Trinity Water Sands - High Wash-300658
Cisco1,630-672

BYarbrough #21 42-337-35504

Tettleton, Steven B. · Montague · 1,299 ft elevation · 4,500 ft TD

FormationMD ftSubsea
Trinity Water Sands - High Wash-350949
Cisco2,306-1,007
CanyonCANYON SAND3,052-1,753
Strawn3,162-1,863
Brazos River3,476-2,177

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.