Estate of De Bie v. Commissioner

56 T.C. 876, 1971 U.S. Tax Ct. LEXIS 91
CourtUnited States Tax Court
DecidedJuly 29, 1971
DocketDocket No. 1912-68
StatusPublished
Cited by41 cases

This text of 56 T.C. 876 (Estate of De Bie v. Commissioner) is published on Counsel Stack Legal Research, covering United States Tax Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Estate of De Bie v. Commissioner, 56 T.C. 876, 1971 U.S. Tax Ct. LEXIS 91 (tax 1971).

Opinion

Atkins, Judge:

The respondent determined deficiencies in income tax against tbe petitioner as follows:

Tear Deficiency
1960 _$25, 345.83
1961_ 68,137.73
1962 _ 73, 729.91
Total _167,213.47

Certain issues having been conceded, tbe only issues remaining for determination are (1) whether certain amounts spent by tbe petitioner in connection with a mine constitute deductible development expenses as claimed by petitioner or nondeductible exploration expenses as determined by the respondent, and (2) tbe value of certain tangible personal property donated by tbe petitioner in 1961 and 1962 to a charitable organization. Certain other adjustments are in issue solely because they depend on tbe proper amount of adjusted gross income.

FINDINGS OF FACT

Some of tbe facts have been stipulated and are incorporated herein by this reference.

Alexia DuPont Ortiz DeBie filed her individual Federal income tax returns for tbe taxable years 1960,1961, and 1962 with tbe district director of internal revenue, Wilmington, Del. Sbe died on February 11, 1963, and E. Kussell Jones was appointed executor of ber estate. At tbe time of tbe filing of tbe petition herein, tbe executor of the estate resided in Wilmington, Del. As a matter of convenience, tbe deceased, Alexia DeBie, shall be referred to as tbe petitioner rather than tbe estate.

In 1953, petitioner acquired a leasehold interest in property known as the “Deer Trail Mine.” During tbe period 1954 through 1962, she operated tbe Deer Trail Mine as a lessee doing business under the name of Ar andel Mining Co.

Tbe mine is located about 5 miles southwest of Marysvale, Utah, which is about 190 miles south of Salt Lake City, Utah. The mine lies on the east side of a range of mountains known as the Tushar Mountains. The mine is in the foothills of the mountains, at a low elevation in relation to the height of the surrounding mountains.

Faulting has been important in the geological history and creation of the Tushar Mountains. There is considerable north-south faulting parallel to the great faults that outline the range. A fault is a fracture in the earth’s surface along which there has been movement of the rock.

When petitioner acquired the mine, the main area of work was an area in the AID tunnel 3,400 feet from the portal of the tunnel. The AID tunnel was a haulage tunnel driven horizontally into the side of the mountain. The portal was at an elevation of approximately 6,900 feet above sea level. The AID tunnel proceeded in a westerly direction about 1,300 feet from the portal and then turned to a northwesterly direction and continued to a point about 5,000 feet from the portal. Five hundred feet vertically above the AID tunnel was the tunnel of the old Deer Trail Mine. This tunnel had a length of several thousand feet. The main workings in the old Deer Trail Mine were 500 feet vertically above and just beyond the 3,400 area of the AID tunnel. Over its history, the old Deer Trail Mine had produced about 190,000 tons of ore, principally gold and silver, with a value in excess of $3 million until it ceased producing during World War II when restrictions prohibited the mining of gold. Vertically above the old Deer Trail tunnel was the Lucky Boy tunnel, which involved ore beds considerably higher in elevation than the old Deer Trail ore bed.

Before she acquired the mine, petitioner, in 1953, requested Quillen Treseder, a geologist and mining engineer employed by Anaconda Co., to examine and analyze the mine and recommend whether money should be spent in further working the 3,400 area of the AID tunnel. On two prior occasions in 1942 and 1952, Treseder had made analyses of the mine for Anaconda. When he examined the mine in 1942, the AID tunnel had been driven only 1,300 feet and most of the old Deer Trail tunnel was still accessible. Prior to Treseder’s examination in 1953, there had been some extraction of ore from the 3,400 area. Based on this and on the known occurrences of ore, he recommended further work in the area. At this time he again examined and considered the old Deer Trail Mine. He was familiar with the ore that had been extracted from it and the approximate locations from which it had been extracted, but had no specific plans to further work the old Deer Trail ore body.

In March 1954, petitioner hired Treseder to operate the mine. Since that time, he has worked continuously as the mine’s sole geologist and engineer. His responsibilities have included recommending to petitioner policies and programs for the mine and subject to petitioner’s approval, carrying these out. During this period until 1963, there had also been from 10 to 15 other people employed in the total operations of the mine.

When Treseder started working at the mine, operations had been underway for a number of months. However, these operations were antiquated and inefficient. For the next 6 to 8 months, work in the mine was concentrated on rehabilitating and mechanizing the mine’s operations to the greatest possible extent.

During the period from 1954 through 1959, the work in the AID tunnel was almost entirely related to the ore (principally lead, zinc, and copper) that had been exposed in the 3,400 area. The 3,400 area contained a mineral deposit of sufficient size, quality, and grade to reasonably justify exploitation with the possibility of profit after the cost of extraction and processing.

Since he began operating the mine in 1954, Treseder, as a geologist, has taken account of a number of considerations in determining which way to go and what to do to locate ore. He has tried to determine what localized the ore in a particular area and the effect of various factors that were exposed in the course of the workings on the presence and location of larger ore occurrences. Some of the factors involved are the presence of veins, fissures, or faulting action, the existence of beds that are receptive to the localization of ore, and the occurrence of silicification or rock alteration. Based upon these various factors Treseder would formulate a projection as to where the ore might be encountered.

From the prior workings in the 3,400 area, Treseder had a general idea of the stratification, fracturing, and Assuring in that area. In the 3,400 area there was a bed of limestone, the Kaibab. Under this was a bed of quartzite, the Coconino, about 450 feet thick. Under the Coconino was another limestone bed, the Hermosa. Limestone beds are generally considered to be host rocks favorable to the deposition of

Prior to 1954, some ore had been, mined from the tunnel level in the 3,400 but no substantial deposits had been disclosed. When Treseder began the workings in the 3,400 area after 1954, varying amounts and varying grades of ore were exposed. This ore occurred in an area of silicification. An area of silicification results from the conversion of a part of a limestone bed into silica. This conversion preceded the deposition of the ore so that ore occurrences in the 3,400 area were associated with the area of silicification. The tunnel level of the 3,400 area was the top of a silicified area.

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Bluebook (online)
56 T.C. 876, 1971 U.S. Tax Ct. LEXIS 91, Counsel Stack Legal Research, https://law.counselstack.com/opinion/estate-of-de-bie-v-commissioner-tax-1971.