Town of Genoa v. Westfall

349 P.2d 370, 141 Colo. 533, 1960 Colo. LEXIS 734
CourtSupreme Court of Colorado
DecidedFebruary 8, 1960
Docket18557
StatusPublished
Cited by15 cases

This text of 349 P.2d 370 (Town of Genoa v. Westfall) is published on Counsel Stack Legal Research, covering Supreme Court of Colorado primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Town of Genoa v. Westfall, 349 P.2d 370, 141 Colo. 533, 1960 Colo. LEXIS 734 (Colo. 1960).

Opinion

Opinion by

Mr. Justice Moore.

Defendant in error was plaintiff in the trial court and we will refer to him as plaintiff or Westfall. Plaintiff in error was defendant in the lower court and will be referred to as the town or Genoa.

Westfall brought the action to enjoin the town from intercepting and diverting water forming the supply source of certain springs on his lands and to recover damages allegedly sustained by him because of the past diversions of said water and the resultant “drying up” of his springs.

The town alleged defenses which included a general denial of all pertinent facts, a claim of ownership and prior right to the water being diverted by the town under the doctrine of prior appropriation, and that the water was not tributary to any stream and belonged to the town because the aquifer from which it was taken was on land belonging to it.

After a lengthy trial the trial court, with commendable care, prepared a detailed analysis of the contentions of the parties and the evidence upon which they were grounded.

The town owns eighty acres of land which is immediately north of the eighty acres upon which Westfall resides and upon which are located the springs which he alleged had been “dried up” by the acts of the town. Westfall also owns 7280 acres lying immediately south and east of the 80 acres upon which his home is located. The controversy between the parties can best be shown by quotations from the findings of the trial court as follows:

*535 “That the Town Eighty is located along the bluffs south of the Rock Island Railroad, the north boundary thereof being at the top of the bluffs and the south boundary at or near the bottom. The Westfall Eighty is immediately south of the Town Eighty, the north half thereof being rather rolling and, from thereon south and east for several miles, the land is comparatively level and good pasture land. The Westfall ranch improvements are bout (sic) 40 rods from the west boundary of the Westfall Eighty and about midway between the north and south boundaries of the Eighty.

“The Court further finds that the land in this part of the State is underlaid with Pierre shale, a formation impervious to water. That in ages past a large river flowing toward the east cut a wide channel in the Pierre shale, forming the bluffs on the north and south sides of the valley through which the Big Sandy now runs. The Ogallala lies above the Pierre shale as originally laid down and is found on top of the bluffs and extending to the north and east. The overburden on the slopes of the bluffs and in the valley consists of weathered Pierre shale, clay, gravel, and wash brought in and deposited by the streams and waters flowing into and through the valley. The alluvium in the bluffs varies in depth from four to thirteen feet, being deeper in the gulches and flatter portions than on the sides of the bluffs.

“That the Town Eighty is very rough, consisting wholly of bluff land not suitable for agriculture and very poor pasture land. The land is very precipitous. From the top of the bluffs to the Westfall north boundary there is a drop in elevation of approximately 125 feet and, from the top of the bluffs to the Westfall improvements, a drop- of approximately 175 feet. Four deep draws or gulches run through the Town Eighty north to south. The two on the west converge on the Westfall Eighty above the Westfall improvements and, north of what has been referred to as the garden plot, curve *536 rather sharply to the west (as shown in Defendant’s Exhibit 4) and then curve around the edge of the garden plot and through a corner of the Westfall corrals and then run in a southerly direction below the Westfall corrals where the draw is joined by the two easterly draws or gulches above mentioned. At the bottom of the gulches on the Town Eighty and through the West-fall Eighty and for some distance beyond water runs in an open ditch with steep banks and a well defined water course in the bottom. The open ditch disappears for some distance in Section 19, the water in times of freshets or large runoffs from melting snows spreads out and flows over a swail, breaks out again in an open ditch at or near the public road between Sections 19 and 30 and continues in a southeasterly direction and joining or being joined by other streams flows into the Big Sandy below Hugo, Colorado. (See aerial photos, Defendant’s Exhibits 5 and Plaintiff’s Exhibit F).

“That, because of the precipitous character of the land and the nature of the soil, rainfall or water from melting snow rapidly finds its way into the gulches either as surface runoff or by percolation and runs down the gulches as surface flow or underflow to the Westfall improvements. The total area thus drained is approximately 100 acres and water falling on the watershed as rain or snow is concentrated or collected and flows through the narrow neck between the Westfall corrals and the garden plot.

“THE DEFENDANT’S CLAIM TO WATER

“The Court finds that one, Givens, obtained U. S. Patent to the North Half of the Southwest Quarter of Section 18 only, in 1886. He, prior to that date, conveyed to McIntyre and Thurlow, and Thurlow conveyed to McIntyre in 1896. McIntyre owned adjoining lands and other lands in Lincoln County and was engaged in the sheep business.

“That there were two well known springs on the North Half of the Southwest Quarter of Section 18; the larger *537 one, which shall be called ‘McIntyre No. 1,’ was located in the second large gulch or draw from the west and approximately 6 or 8- rods from the north boundary of said land. This was a contact spring, breaking out at or near the top of the Pierre shale as originally laid down. The source of the water being water collected in the aquifer above the Pierre over an indefinite area to the north and east and breaking out through the overburden at the bottom of the gulch and flowing down the gulch for some distance toward the Westfall Eighty. The spring was directly tributary to the stream.

“McIntyre Spring No. 2 is located directly east of McIntyre No. 1 about 500 feet distant in the third draw. It, too, is a contact spring of the same nature as Spring No. 1 and flowed directly into the water course in the draw and is tributary to that stream. The water from this spring, together with other waters, converged with the waters from gulches or draws Nos. 1 and 2 below the Westfall improvements. Springs Nos. 1 and 2 are each on the west side of their respective gulches.

“The Court further finds that prior to the entry of the South Half of the Southwest Quarter of said Section 18 McIntyre established a sheep camp on the North Half of said Quarter just below Spring No. 1. That he built a dam in the gulch about 400 feet below the spring, put in watering troughs, built a herder’s shack and other improvements and for a number of years and until 1910 or 1911 used the land as headquarters for his sheep grazing business. That he ran upwards of 4000 sheep and the water from the spring was used for watering his sheep and other domestic purposes on said land.

“That, in 1919, Wm. M.

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Bluebook (online)
349 P.2d 370, 141 Colo. 533, 1960 Colo. LEXIS 734, Counsel Stack Legal Research, https://law.counselstack.com/opinion/town-of-genoa-v-westfall-colo-1960.