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

1,000-0-1,000-2,000-3,000-4,000SUBSEA FTA2,087 FT ELB2,117 FT ELSan AndresSan AndresCanyonCanyonCanyon ReefCanyon Reef

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.

  • ASalt Creek Field Unit #H 65W
  • BSalt Creek Field Unit #D 74W
FormationAB
San Andres1,073 MD 1,0141,011 MD 1,106
San Angelo—265 MD 1,852
Glorieta—225 MD 1,892
Clear Fork—69 MD 2,048
Wichita-Albany—-773 MD 2,890WICHITA ALBANY
Wolfcamp—-1,727 MD 3,844
Cline—-3,595 MD 5,712
Canyon-3,796 MD 5,883-3,616 MD 5,733
Canyon Reef-4,153 MD 6,240-4,193 MD 6,310

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.