WELLS · CROSS-SECTION

2 wells, subsea datum

West to east, 0.1 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. Dashed lines join the same normalized formation in neighbouring wells; nothing is interpolated. Where tops come from →

1,000-0-1,000-2,000-3,000-4,000SUBSEA FTA2,496 FT ELYatesSan AndresGlorietaClear ForkWichita Albany - Over PressuredWichitaWolfcampColeman JunctionCiscoCanyonStrawnB2,479 FT ELYatesSan AndresGlorietaClear ForkWichitaWichita Albany - Over PressuredWolfcampColeman Junction

reported topsame formation, neighbouring wells

The tops, as filed

ASacroc Unit #133-7 42-415-35323

Kinder Morgan Production Co LLC · Scurry · 2,496 ft elevation · 7,500 ft TD

FormationMD ftSubsea
YatesYATES - HIGH FLUIDS AND/OR GAS F8661,630
San AndresSAN ANDRES - HIGH FLOWS, H2S, CO1,647849
Glorieta2,46630
Clear ForkCLEARFORK2,664-168
Wichita-AlbanyWICHITA ALBANY - OVER PRESSURED4,309-1,813
Wichita-AlbanyWICHITA4,309-1,813
Wolfcamp4,748-2,252
Coleman JunctionCOLEMAN JUNCTION - POSSIBLE LOST4,748-2,252
Cisco6,720-4,224
Canyon6,925-4,429
Strawn7,121-4,625

BSacroc Unit #133-4 42-415-35455

Kinder Morgan Production Co LLC · Scurry · 2,479 ft elevation · 7,800 ft TD

FormationMD ftSubsea
YatesYATES - HIGH FLUIDS AND/OR GAS F8051,674
San AndresSAN ANDRES - HIGH FLOWS, H2S, CO1,605874
Glorieta2,42851
Clear ForkCLEARFORK2,626-147
Wichita-AlbanyWICHITA4,297-1,818
Wichita-AlbanyWICHITA ALBANY - OVER PRESSURED4,297-1,818
Wolfcamp4,740-2,261
Coleman JunctionCOLEMAN JUNCTION - POSSIBLE LOST4,740-2,261

About this data

Formation tops and elevations from the RRC dbf900 wellbore file (completion filings), names normalized to the formations registry; well identity and location from the permit 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.