St UT v. USA, et al
Filing
822
MEMORANDUM DECISION: The court sets the lake-wide boundary at the lower of (1).2 feet below Compromise Elevation of 4488.95 or (2) the Meander Line. This boundary shall be applied to all parcels that have not already agreed to a boundary through settlement. Signed by Judge Dale A. Kimball on 3/15/13. (jlw)
______________________________________________________________________________
IN THE UNITED STATES DISTRICT COURT FOR THE DISTRICT OF UTAH
CENTRAL DIVISION
STATE OF UTAH, by and through it
DIVISION OF FORESTRY, FIRE AND
STATE LANDS,
Plaintiff,
MEMORANDUM DECISION AND
ORDER
Case No. 2:97CV927DAK
vs.
UNITED STATES OF AMERICA;
DEPARTMENT OF THE INTERIOR;
BUREAU OF RECLAMATION; ELUID
MARTINEZ, in his official capacity as
Commissioner; BUREAU OF LAND
MANAGEMENT; SALLY WISELY, in
her capacity as Utah State Director, BLM;
RICHARD W. DAVIS; JOHN DOE and
MARY DOE; et al.,
Judge Dale A. Kimball
Defendants.
This matter is before the court on the determination of a lake-wide boundary elevation for
Utah Lake (referred to as “Phase 1"). The parties have submitted evidence and fully briefed the
issue. On December 12, 2012, the court held oral arguments on the Phase 1 issue. At the
hearing, the State of Utah was represented by Michael S. Johnson, the Landowner Defendants
were represented by Robert C. Fillerup, and the Intervenors were represented by Jorro Walker.
The court took the matter under advisement and agreed to issue its order after the parties had
time to complete additional settlements. The court has allowed that time to expire. After
carefully considering the evidence submitted, the arguments advanced by the parties, and the law
and facts relevant to the issue, the court issues the following Memorandum Decision and Order.
BACKGROUND
After making several legal rulings in this matter, United States District Court Judge Dale
A. Kimball referred the case to Special Master Michael Goldsmith pursuant to Rule 53(a) (1)(B)
of the Federal Rules of Civil Procedure. The court’s Order of Reference tasked the Special
Master with taking evidence relevant to the boundary of each parcel of property in which the
boundary is still in dispute, making findings as to the historic usage, title, and possession of each
parcel, and issuing a report recommending the proper boundary for each of the parcels.
The parties had a trial in this matter before Special Master Michael Goldsmith on August
1, 2006. At the trial, the State presented substantial evidence of monthly lake level data, expert
scientific analysis of the water levels’ effects on soils and plant growth, historical plats, and
photographs. The Special Master found the State’s evidence “comprehensive” and
“overwhelming.” The Landowner Defendants, however, supplied no evidence of their historic
usage, title, and possession. To allow the Landowner Defendants another opportunity to submit
relevant evidence, Special Master Goldsmith laid out a two-phase procedure for addressing the
issues in this case: Phase 1 involves the determination of a lake-wide boundary elevation based
on evidence submitted by the parties; and Phase 2 involves projecting that lake-wide boundary
onto each remaining parcel in dispute. The court approved and adopted the Special Master’s
First Report & Recommendation.
After the Special Master’s First Report & Recommendation, the Landowner Defendants
submitted evidence of use and possession dating back to the 1930s. The State’s evidence
providing water levels over the decades demonstrated that the lake levels were lowest in the
2
1930s, 1960s, and 1990s. Thus, testimony regarding the water levels in the 1930s would be
uncharacteristically low. In his Second Report & Recommendation, Special Master Goldsmith
rejected the Landowners’ evidence because it was too remote in time from statehood. The
Special Master gave the Landowners another opportunity to submit evidence during briefing on
Phase 1. The court approved and adopted the Special Master’s Second Report &
Recommendation.
The parties submitted their evidence for the Phase 1 determination of a lake-wide
boundary to Special Master Goldsmith. However, he was unable to make his ruling on the Phase
1 boundary before his death. This court held a status conference on January 21, 2010, at which
the parties asked the court to delay ruling on Phase 1 while they attempted to settle as many
parcels as possible. The parties have engaged in extensive settlement efforts for the past three
years.
DISCUSSION
Based on the court’s prior rulings, the parties agree that the controlling boundary test in
this case was established in the Utah Supreme Court’s Jacobsen decisions. See Provo City v.
Jacobsen, 176 P.2d 130 (Utah 1947); Provo City v. Jacobsen, 181 P.2d 213 (Utah 1947); Provo
City v. Jacobsen, 217 P.2d 577 (Utah 1950). This test looks to evidence of statehood-era use and
possession to ascertain the location of the statehood vegetative high water mark, below which
valuable agricultural plants cease to grow. Jacobsen III, 217 P.2d at 578. Jacobsen explained
that the vegetative line/boundary is a mark impressed upon the soil over several years based on
the frequency and duration of inundation and its effects on the soil. Jacobsen, 176 P.2d at 133;
Jacobsen III, 217 P.2d at 578.
3
To meet the Jacobsen test, Special Master Goldsmith afforded the Landowner
Defendants another opportunity to submit evidence during briefing on Phase 1, but they did not.
The State continues to rely on the evidence it presented at the initial trial to meet the Jacobsen
test. The State submits that its evidence, even when conservatively read, demonstrates that the
ground suitable for agricultural cultivation extended no lower than .2 feet below Compromise
Elevation at statehood.
This court has recognized that the State’s evidence, which identifies statehood-era water
levels and analyzes their effects upon soils in light of plant water needs and tolerances, is
consistent with and is the kind of evidence called for under the controlling Jacobsen boundary
test. The State’s evidence that the boundary be set at a level of .2 feet below the Compromise
Elevation is based upon a conservative reading of the evidence in the record. The evidence in the
record could support a boundary setting at a higher elevation. The State’s experts indicate that
the statehood boundary was located somewhere between .2 feet below Compromise and .4 feet
above Compromise. For simplicity’s sake, this calculation does not include orthometric
corrections, which the experts believe would have pushed the estimates higher. Moreover,
although the State believes the evidence supports a finding that the Compromise Elevation is
located at 4489.34 feet above sea level, it has agreed to use a lower level, 4488.95, for the
Compromise Elevation.
The minus .2 feet below Compromise level lies below the 1885 Compromise Elevation,
which was not tied to any specific elevation above sea level, and, in many locations around the
lake, below the meander line as well. The meander line is not an elevation specific line, and for a
few Landowner Defendants, the meander line is located lower than .2 feet below Compromise.
4
The meander line is a metes and bounds surveyed line that does not follow the contour or
elevation of the lake bed. The State submits that it has never sought land above the meander line
regardless of elevation. The State, therefore, urges that the statehood boundary be set at the
lower of .2 feet below Compromise Elevation or the meander line, which benefits the
Landowners.
The Landowners have previously disagreed with the idea of using statehood era lake
levels to set the boundary. Nevertheless, the Landowners state that the evidence submitted by the
State, coupled with the 4481 Stipulation, sets the boundary at statehood no higher than 2.4 feet
below Compromise Elevation. The Landowner Defendants argue that if statehood era water
levels are going to be used, they should have the benefit of the lowest elevation of the water’s
edge for those years. In the 4481 Stipulation, the parties agreed that the landowners used the land
“to the water’s edge.” The lowest monthly water level during the statehood era was in November
1895 at 2.4 feet below compromise. Thus, the Landowner Defendants contend that this is the
level where the boundary should be set.
However, picking the lowest monthly water level is not in accordance with the Jacobsen
test. The Jacobsen test focuses on averages over several years, not the lowest monthly reading.
In addition, the fact that the Landowners used to the water’s edge is helpful in determining usage,
but it is not determinative of a boundary when the evidence demonstrates significant monthly
fluctuations of lake levels. The State’s experts provide persuasive testimony regarding usage in
relation to the water fluctuations.
As a quiet title plaintiff, the State has the burden to prove the claimed boundary by a
preponderance of the evidence. The State has produced substantial evidence from the statehood
5
era which fits the analytical framework set out in the Jacobsen decisions and this court’s prior
orders. This evidence stands unchallenged and unimpeached. Because the Landowner
Defendants have not produced evidence of statehood-era use and possession, the boundary is
must properly be based on the State’s evidence. The court concludes that the State has met its
burden. Therefore, the court agrees with setting the boundary at the State’s requested level.
CONCLUSION
Based on the above reasoning, the court sets the lake-wide boundary at the lower of (1)
.2 feet below Compromise Elevation of 4488.95 or (2) the Meander Line. This boundary shall be
applied to all parcels that have not already agreed to a boundary through settlement.
Dated this 15th day of March, 2013.
BY THE COURT:
____________________________________
DALE A. KIMBALL,
UNITED STATES DISTRICT JUDGE
6
Disclaimer: Justia Dockets & Filings provides public litigation records from the federal appellate and district courts. These filings and docket sheets should not be considered findings of fact or liability, nor do they necessarily reflect the view of Justia.
Why Is My Information Online?