TOOLS · CROSS-SECTION · TEXAS

2 wells, subsea datum

West to east, under 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. 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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2,000-0-2,000-4,000SUBSEA FTA3,365 FT ELB3,363 FT ELRustlerRustlerDelawareDelawareCherry CanyonCherry CanyonBone SpringBone SpringWolfcampWolfcamp

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.

FormationALt. Gibson 1 State EBCount Fleet 48 State I
Rustler3,165MD 2002,913MD 450
Delaware1,543MD 1,8221,571MD 1,792
Cherry Canyon542MD 2,823538MD 2,825
Bone Spring-2,026MD 5,391-1,994MD 5,357
Wolfcamp-5,000MD 8,365-5,002MD 8,365

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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

Cimarex Energy Co. · Culberson · 3,365 ft elevation · 11,580 ft TD

FormationMD ftSubsea
Rustler2003,165
Delaware1,8221,543
Cherry Canyon2,823542
Bone Spring5,391-2,026
Wolfcamp8,365-5,000

Cimarex Energy Co. · Culberson · 3,363 ft elevation · 15,000 ft TD

FormationMD ftSubsea
Rustler4502,913
Delaware1,7921,571
Cherry Canyon2,825538
Bone Spring5,357-1,994
Wolfcamp8,365-5,002

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.