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How deep are water wells in Loraine, Texas?

Only 12 home water wells in and around Loraine, Texas have been reported since 2001, so treat this as a rough guide: the middle half are 181 to 241 feet deep (median 228 ft). Most end near or below the base of the Dockum, or of the Ogallala where there is no Dockum (58%), and 42% end at or just below the base of the Ogallala, in the top of the Dockum, according to the state's High Plains Aquifer System model (TWDB). Most of these reports do not say where the water enters, so the formation is a rough guide. Estimated cost of a complete well at the median depth: $8,000 to $20,000.

This page is based on fewer than 30 wells, so it is kept out of search engines until more reports come in. Treat every figure as a rough guide.

Updated every day from Texas Water Development Board driller reports. Last update: November 11, 2026, using the state file of November 10, 2026.

See the wells and layers at an exact pointMitchell County
What is under Loraine, TexasUnderground column at the center of Loraine: median well 228 ft, middle half 181 to 241 ft, water at 68 ft, and the layers of the state's model with their thickness.Dockum: 0 to 196 ftDockumBelow the base of the model0100200300ftGround level · 2,300 ft above sea levelMedian well: 228 ftWater standing in the well from 68 ftWater level68 ftMiddle half181–241 ftMedian well228 ft

Under Loraine, Mitchell County

Layers at the center of Loraine from TWDB's High Plains Aquifer System model (half mile cells, read here on a grid of about 1.2 by 1.4 miles), at true depth scale. The well and the water are the median of 12 real wells.

Home wells in and around Loraine

Each dot is a home well from a state driller report, colored by depth. Tap one for its details and official report. Tap an empty spot to see what is under that point.

See underground

Well depth (ft)

  • <100
  • 100
  • 200
  • 300
  • 400
  • 600
  • 800+

Dashed line: Loraine and about 2 miles around it

Key figures

Typical depth (middle half)
181 to 241 feet
Median depth
228 feet
Deepest 10% are past
276 feet
Water level (median)
68 feet
10 wells
Wells used
12
Since 2001
Inside the city limits
2
the rest within 2 miles
All years on file
12
median 228 ft, since 2005
Confidence
Few wells (10 to 29)

When the wells were finished, the water stood a median 68 feet below the surface (10 wells), well above the bottom: the typical well holds about 160 feet of water.

What is under Loraine, TexasUnderground column at the center of Loraine: median well 228 ft, middle half 181 to 241 ft, water at 68 ft, and the layers of the state's model with their thickness.Dockum: 0 to 196 ftDockumBelow the base of the model0100200300ftGround level · 2,300 ft above sea levelMedian well: 228 ftWater standing in the well from 68 ftWater level68 ftMiddle half181–241 ftMedian well228 ft
Layers at the center of Loraine from TWDB's High Plains Aquifer System model (half mile cells, read here on a grid of about 1.2 by 1.4 miles), at true depth scale. The well and the water are the median of 12 real wells.

Which formation do wells in Loraine draw from?

Most end near or below the base of the Dockum, or of the Ogallala where there is no Dockum (58%), and 42% end at or just below the base of the Ogallala, in the top of the Dockum, according to the state's High Plains Aquifer System model (TWDB). Read that as the base of the Ogallala or the top of the Dockum, not a certainty: where our method names the Dockum, the state's own record agrees only about 33% of the time (61% for wells with a screened interval), and most of the others are recorded as Ogallala wells. Most of these wells have no screened interval on their report, and for those the method is only a little better than always answering the Ogallala (it matches the state's record about 65% of the time, against 58%): read the formation as a rough guide.

Going by the bottom of the hole instead of where the water enters, 67% reach near or below the base of the Dockum, or of the Ogallala where there is no Dockum. 67% of the wells bottom out near or below the base of the Dockum, or of the Ogallala where there is no Dockum in the model, often within tens of feet of it; older Permian red beds lie there, and the state usually records these wells as Ogallala or Dockum wells.

Layer (state's model)ShareWellsTypical depth (ft)
Near or below the base of the Dockumor of the Ogallala58%7228–242
Dockumat or just below the base of the Ogallala42%5120–220

Only 25% of these wells have the water-bearing interval on their report (reports before about 2012 rarely do). For the others we use the bottom of the hole, which tends to read one layer deeper than where the water actually comes from.

The layers under the center of Loraine

From the state's model, at 2,300 feet above sea level. These are the model's depths at that one point, not those of any particular lot.

Depths in feet below ground.
Layer (state's model)Top (ft)Bottom (ft)Thickness (ft)
Dockumred mudstone, sandstone and conglomerate0196196

Depth over time

Too few wells per period in and around Loraine to compare depth over time. Since 2005, 12 home wells have been reported, with a median of 228 feet.

PeriodMedian depth (ft)Wells
2001–2005under 10 wells1
2006–2010under 10 wells4
2011–2015under 10 wells3
2016–2020under 10 wells1
2021–2025under 10 wells3

What a well costs in Loraine

At the median depth for Loraine (228 feet), a complete home well would cost roughly $8,000 to $20,000: $25 to $60 per foot for drilling, casing and seal, plus $2,500 to $6,500 for the pump, pressure tank, controls and hookup at the well. Across the whole middle half of depths (181 to 241 feet) the range runs from $7,000 to $21,000. This is TerraFunded's estimate from published Texas prices, not a quote, and it leaves out trenching and the line to the house. Get prices from at least two licensed drillers.

Where it sits

Nearby places

Median depth of home wells in each place.

All Texas cities and towns

Common questions

How deep do you have to drill a well in Loraine, Texas?

Only 12 home water wells in and around Loraine, Texas have been reported since 2001, so treat this as a rough guide: the middle half are 181 to 241 feet deep (median 228 ft). One in ten goes past 276 feet. The depth a given tract needs depends on where it sits and what layers the driller hits.

What aquifer or formation do wells in Loraine draw from?

Most end near or below the base of the Dockum, or of the Ogallala where there is no Dockum (58%), and 42% end at or just below the base of the Ogallala, in the top of the Dockum, according to the state's High Plains Aquifer System model (TWDB). Read that as the base of the Ogallala or the top of the Dockum, not a certainty: where our method names the Dockum, the state's own record agrees only about 33% of the time (61% for wells with a screened interval), and most of the others are recorded as Ogallala wells. Most of these wells have no screened interval on their report, and for those the method is only a little better than always answering the Ogallala (it matches the state's record about 65% of the time, against 58%): read the formation as a rough guide. This is an estimate from the state's regional model, not a survey of the lot.

How much does a water well cost in Loraine?

At the median depth (228 feet), a complete well would cost roughly $8,000 to $20,000, by TerraFunded's estimate from published Texas driller prices. The real price comes from a licensed driller's quote.

How deep is the water in Loraine?

When the wells were finished, the water stood a median 68 feet below the surface (10 wells), well above the bottom: the typical well holds about 160 feet of water. The level moves with drought and from one well to the next.

Do I need a permit to drill a well in Loraine?

Loraine is inside the Lone Wolf Groundwater Conservation District. Groundwater conservation districts in Texas can require registering or permitting a new well, keeping set distances from property lines and other wells, and paying fees. Rules differ from district to district: ask the district before drilling.

How these numbers are made

We count new and replacement domestic (home) wells whose coordinates fall inside the place boundary or within 2 miles of it. We use the last 10 years when there are at least 30 wells; otherwise all since 2001. The median is the middle well and the middle half runs from the 25th to the 75th percentile.

To tell which layer a well draws from, we take the ground elevation at its location, subtract the depth of the interval where water enters (or the bottom of the hole when the report does not give one) and see which layer of the state's model that point falls in.

Only 25% of these wells have the water-bearing interval on their report (reports before about 2012 rarely do). For the others we use the bottom of the hole, which tends to read one layer deeper than where the water actually comes from.

How well it works: In 22,814 wells in the Texas part of the state's High Plains Aquifer System model (the Panhandle, the South Plains and the Permian Basin) where the State of Texas recorded the aquifer, the formation our method says the well draws from (as grouped on these pages) is the one the state recorded in about 75% of them; when it names the Dockum (4,542 wells), the state's record agrees only about 33% of the time, and most of the others are recorded as Ogallala wells.

  • The layers come from the Texas Water Development Board's High Plains Aquifer System model, with half mile cells, read here on a grid of about 1.2 by 1.4 miles. It is a regional model, not a survey of any lot.
  • The state's model has half mile cells; we read it on a grid of about 1.2 by 1.4 miles, Texas part only. Layers from version 1.01 (2015); the 2025 extension (1.02) did not change them. It is not a survey of any lot, so we give ranges.
  • Figures go by four groups: Ogallala; Pecos Valley; Edwards-Trinity and Rita Blanca (Cretaceous rock under the Ogallala; the Rita Blanca alone matched the state 19%); Dockum (upper and lower together: the state's codes almost never say which). The Edwards-Trinity group joins three aquifers in different places (High Plains around Lubbock, Plateau around Midland and Odessa, Rita Blanca in Dallam and Hartley): county and place pages name the local one where they can.
  • Dockum: when our method names the Dockum, the state's record agrees only 33% of the time over all years (61% for wells with a screened interval, which is 93% of home wells of the last 10 years); most of the rest are recorded as Ogallala wells. The median well we put in the Dockum ends about 18 ft under the base of the Ogallala as the model draws it. So these pages say "at or just below the base of the Ogallala, in the top of the Dockum", never a certain formation. The state's own 2025 report on this model says depth alone overstates the upper Dockum.
  • "Near or below the base" means the well ends near or below the base of the Dockum, or of the Ogallala where there is no Dockum (Permian red beds; Gray, Carson, Donley, Moore and north Potter counties). Half of these wells end within about 51 ft of the base, and the state usually records them as Ogallala or Dockum wells. That is not an error: the model simply ends there.
  • For old wells without a screened interval (bottom of the hole) the method is only a little better than always saying Ogallala (65% against 58%); with an interval it is 89% against 80%. Figures over all years carry that weakness; last 10 years figures rest almost entirely on intervals.
  • We never use the model's water levels. The water level on this page is the one each driller measured when the well was finished.

These are depths of real wells drilled nearby, not a promise about any property. Groundwater can change over short distances and with drought. A licensed water well driller can tell you what to expect on a specific tract.

Read the full methodology · Download the data (CSV, CC BY 4.0)

How to cite

TerraFunded (2026). Texas Well Atlas: Underground. From Texas Water Development Board driller reports and groundwater availability models (data as of November 10, 2026). https://terrafunded.com/wells/places/loraine-tx. License CC BY 4.0. https://doi.org/10.5281/zenodo.24126380.

Sources