*1 The JOHN G. AND MARIE STELLA
KENEDY MEMORIAL FOUNDA Corpus TION and Christi Diocese Church, the Roman Catholic Petition ers,
v. DEWHURST, David Commissioner of Office, the General Land and The Texas, Respondents. State of No. 99-0667. Supreme Court of Texas.
Argued April Aug. Decided Rehearing Denied Dec.
269 Ramirez, Gary W. E. Roberta Nye, Paul Hoblit, Dohse, Gonzales & Cor- S. Chavez Ratliff, Akin Christi; H. Shannon pus Feld, Austin; Hauer & Gump Strauss Forestier, Knisley, Thomas J. Marc O. Houston; Lochridge Kilgore, <& McGinnis Leshin, Law Kleburg Richard L. Hatchell, Antonio; Firm, A. and Mike San Hatchell, P.C., Tyler, for Petitioner. McKetta, III, Vaughan, Ben F. J. John Cabaniss, Allen, III, Kathryn Boyce E. C. McFarland, Dougherty B. John Graves Austin; and John Moody, & Cor- Hearon Tex- of the State of nyn, Attorney General Austin, as, Respondent. opinion of delivered the
Justice HECHT
Court,
in which Chief Justice
OWEN,
PHILLIPS,
Justice
Justice
JEFFERSON,
O’NEILL,
Justice
joined.
RODRIGUEZ
Justice
opinion
in this case
issuing
After
2000,1
petition-
granted
we
December
and entertained
rehearing2
motion for
ers’
1, 2001).
(March
2000).
(Dec.
Sup.Ct.
44 Tex.
J.
Sup.Ct.
J.
Tex.
argument
which,
oral
a second time.3
jointly
now
own
as
property
We
shown
opinion
judgment
withdraw our earlier
maps,
the appended
comprises
tracts
two
following
and issue the
opinion
lying just
roughly
of Padre
west
Island
the Court.
halfway
Corpus
between
Christi and Port
*3
tract,
Isabel. One
called La
or
Barreta
The
private
State and a
landowner
Barreta”,
“Big
conveyed
the
was originally
dispute the location of the shoreline bound
by King
Spain
IV of
in
and
Charles
1804
ary of two early nineteenth century land
1809 to
Jose
Balli
Lieutenant
Francisco
grants, one by Spain and the
by
other
(who,
aside,
as an
nephew
historical
was a
State,4,
In Luttes v.
Mexico.
we deter
Balli,
of Padre
grantee
Nicolas
the
Pa-
of
mined that the
of
two sovereigns
law those
Island).
tract,
dre
The other
Las
called
governing such
grants was
a shoreline
Motas de la Barreta or the “Little Barre-
is to be found
daily
where the mean
ta”,
adjacent
Big
is
the
Barreta to
is,
high water
average
level—that
of
originally
by
north and
conveyed
was
daily highest water
levels—reaches the
Tamaulipas
Mexican State
to
1834
mainland. Now we are asked to decide
Leonardo
The 1804 grant
Salinas.
was
whether and how the civil law determined
lost, but a
patent
later
the State
in Luttes applies
present
shoreline
confirming,
conveyance
Texas
de-
boundary dispute.
The lower courts
Big
scribed the
Barreta’s eastern bound-
agreed with the
State
shoreline
ary in the same words used to
describe
should be located without reference to
boundary
Little
eastern
in the
Barreta’s
daily high
water levels because of
grant
Laguna
waters of the
—“the
problems measuring
those levels in
State,
course,
Madre”.6 The
owns the
Laguna
Madre
near
land at issue
submerged land and the shore
between
and instead placed
as far
roughly
inland as
property
Foundation’s
and Padre Island.
storms,
water ever reaches in ordinary
The
dispute
Foundation and the State
on the
based
historical record.5 We dis
boundary along
location of the shoreline
and
agree
hold instead that the civil law as
nine
edge
miles of the eastern
of the Foun-
determined in
applies
here and re
Locating
boundary
property.
dation’s
quires that the
boundary
shoreline
this
by
is made difficult
the nature of the sea-
case,
like all
governed
others
civil
part
Lagu-
water inundation of this
daily
be set at
measured mean
na
parties’ respective posi-
Madre. The
water levels. We therefore reverse the
starkly.
tions conflict
The Foundation
judgment
appeals
court
and re
claims that the
is the
bank
west
mand the case
court
trial
for rendi
of the Intracoastal
where water
Waterway,
of judgment
tion
in accordance with this
always
present
has
been
since it
opinion.
dredged in
The
State claims
I
six
west
boundary is about miles to the
The
at a
a
slight
John G. and Marie Stella
bluff line marked
rise
Kenedy
changes
vege-
elevation
in terrain
Memorial Foundation and the
and
Corpus
tation,
present
Diocese of
Roman
is
most
Christi
Catholic
where water
Foundation”)
(collectively,
days.
Church
“the
once or
for a few
What
year
twice a
(Tex.Civ.
Id. at 456.
Spohn,
6.See State
83 S.W.
v.
d).
App.-Austin
writ ref
(1958).
4. 159 Tex.
324 S.W.2d
5.
has
brought
present
inches;
occur-
infrequent,
in conditions
a few
change
head
local
than
is
Madre,
weeks,
which has remained
or months
ring
days,
several
vicinity
hundred
the same
for two
depending on the area. The rest of
year,
importance
years,
rather the increased
dry,
but
boggy,
time
area
barren
production
the area. The
gas
mud-flat,
of oil and
vegetation except
devoid of
35,000
disputed area totals about
acres.
the mud-
leathery
perimeter
algae.
flats,
gets
ever
which is
far as water
“Mother
translated
storms,
ordinary
a “bluff’ marked more
Lagoon”,
prescribed
whose waters were
of a
less
a small
distinct rise
foot
Spain
disputed
Mexico to mark the
*4
change
and a
or more in elevation
distinct
estuary
a
west
boundary, is narrow
the
ground
vegetation
and
conditions.
extending
side of Padre Island
some
miles from
Christi to Port Isabel.
Corpus
offered,
The State
and the lower courts
of
Laguna
open
The
Madre is
to the Gulf
on,
the
regarding
relied
historical evidence
at both ends but sheltered from
Mexico
and
Big
treatment of the
Barreta
Little
along
Padre
length by
the Gulf
its
Island.
survey
An 1809
grants.
Barreta
areas,
adjacent
In
the
many
including
by
Margil
Big Barreta
Antonio
Cano
property,
slightly
Foundation’s
is
above
boundary approximate-
showed an eastern
The
wa-
presence
depth
sea level.
and
of
ly at the
bluff line
the State now
same
ter in
of
Laguna
gov-
most
the
Madre is
boundary
argues should mark the eastern
by
erned not
astronomic tidal forces from
property.
the Foundation’s
Grantee
of
insulated,
by
which it is
like those exerted
immediately
convey-
Balli
for
petitioned
sun,
and
by meteorological
moon
of
area
of the bluff
ance
an elevated
east
open,
forces to which it remains
like the
line that
inundated and was
was seldom
wind
In
pressure.
and barometric air
area, now
grazing.
suitable for
This
called
much
Laguna
including
Rincon,
Mesquite
was rather like
dispute,
area in
variations water levels
nearly
Madre
island
and
minuscule,
daily
due to
tidal forces are
area now in
by
dispute.
surrounded
entirely by
masked almost
variations
Because it could often be reached
by atmospheric
caused
forces. The water
Big
narrow
from the
Barreta
isthmus
daily,
does not advance and
as one
subside
flats,
through the mud
it was useless
facing
open
thinks of a shore
sea. The
granted
therefore
anyone else
was
actually
uphill
wind can
blow water
so
visualization,
for
we refer
(Again,
Balli.
it is
at
deeper
sometimes
elevations
appended maps.)
the reader
places,
than at
At
the Laguna
lower ones.
petition,
which was
survey
Balli’s
constantly
Madre is
inundated with seawa-
indicate —we will discuss this
granted, may
deep,
ter
for
deep enough
several feet
in due
that Balli did not
course—either
place,
waves and boats. One such
“the
think or was at least unsure that
Hole”,
is near the northeast corner of
grant conveyed anything east of
bluff
another,
property;
Foundation’s
“the
line,
he
measur-
or that
cared most about
Hook”,
corner
the southeast
for
As
however,
ing
grazing.
what land
suitable
property.
places,
At other
in-
Barreta,
survey
the Little
an 1834
for
area
cluding east
the Foundation’s
triangle
Domingo
la Fuente omitted
it is
de
property,
impor-
inundation is—and
of land on
southeast corner
tant
these
character-
precise
to understand
is,
into the
rectangular
tract which extended
regular,
periodic
istics—
recurrent,
Madre and was unsuitable
continually
opposed
sense of
grazing, and added to the northeast corner
firmed Humble
Refining
Oil &
Co. v.
a triangle of land of approximately the Sun
Regarding
Oil Co.7
the location of the
inundated,
same size that
shoreline,
was not
so that
the Fifth
acknowledged
Circuit
grantee
Salinas would have the full
that it was required to apply Texas courts’
grazing
amount of
land that he
had re-
understanding of civil
which it be
quested.
survey
Another
Big
Bar-
mistakenly, as it turned out sever
lieved—
reta in 1882 and the Little Barreta in
years
1879 al
later when we decided the mat
Cocke,
by J.J.
survey
Big
ter —to be that the
highest
shoreline is the
Barreta
around 1907
F.M. Maddox—all
level
reached
the water in winter.
done when grazing
was all that mattered—
we
held Luttes v. State that a civil
never included
area east of the bluff
law shoreline is the mean daily higher high
line in the
property,
level,
landowners’
and the water
not the .highest water level.8
owners at those times do not appear to We will have much
say
more to
about both
objected.
have
cases,
exact
never
these
but for now it is important
appears to have been at issue.
merely to
their place
note
in the sequence
of events leading up
present
litiga
The State also offered evidence that the
*5
tion.
predecessors
Foundation’s
in interest affir-
matively treated the bluff line as
A
the
mean daily higher high tide —which
boundary of
property
their
until the mid-
the parties agree in
synony-
this case is
twentieth century, and that
the Founda- mous with mean daily higher high water—
tion did not render the mud flats for ad is
calculated
averaging
highest
the
ele-
valorem taxation until 1987. The trial
vations
reached
water each day over a
court excluded this evidence on
theory
the
tidal epoch
years.
course,
of 18.6
Of
as we
that later owners’
Luttes,
actions were
recognized
irrelevant
in
water level data is
in determining
original
the
intent of the
coast,
not available at all locations on the
sovereigns expressed in
grants.
the
and where it is available may
only
cover
Foundation contends that
part
the evidence
lengthy
of the
epochal cycle. But
only
shows
predecessors
that its
in inter-
averages may
nevertheless be obtained
mostly
est cared
about land
extrapolation
available,
usable for
from data that is
grazing while maintaining
known,
their claim to
adjusting for
cyclical variations.
the waters of
Laguna
Madre.
At times on the Texas coast there are two
daily high
daily
tides and two
low tides.
1949,
Co.,
Sun Oil
to whom the State
Mean higher high
average
tide is an
of
had leased the minerals in part of the now
of the daily levels. Mean
area,
disputed
sued the Foundations’ pre-
high tide is an average of both high levels.
in
decessors
interest and Humble Oil <&
This distinction is immaterial in areas of
Co.,
Refining
to
they
whom
had leased the
the Laguna Madre where tidal influences
area,
minerals
the same
to determine
daily
fluctuations
water levels are
whose lease was valid.
position
Humble’s
quite
Thus,
ordinarily
small.
purposes
was not that
mud
originally
flats had
case, daily
of this
higher high water is
conveyed
landowners,
been
but that
indistinguishable
daily high
from
water.
they had since accreted to the mainland.
rejected
1995,
The federal district court
Hum-
Prior to
surveying regulations pro-
contention,
ble’s
and the Fifth
af- mulgated by
Circuit
the General Land Office
(5th Cir.),
500,
reh’g,
7. 190 F.2d
(1958).
191 F.2d
8. 159 Tex.
The Foundation has on a relied ly Ma- basis waters *6 begun in 1984 Matt and Bill Claunch Indeed, prin- of dre.” another the State’s They high Lothrop. used water measure- reaches cipal testified that water witnesses ments, but of picking particular instead no than or the bluff fine more once twice data, the they level shown which few year days. then for a hours and might the contest feared State later But uncontroverted evi- there also accuracy as to opposed methodology, the bluff that some areas between dence necessitating thereby expensive another inun- Waterway and were the Intracoastal survey, they level than higher used a year. forty percent much dated as as could prove. State ever The level, course, of for the better jury found Claunch/Loth- They surveyed State. area on the daily higher at or rop line is above mean assumption high that the mean water level tide, it is. Yet high concedes State was one foot above the National Geodetic to question answer whether (NGVD). Vertical Datum of 1929 All of higher tide could be with determined the area on the east side of the Founda- accuracy in area of the reasonable property, upland jury tion’s “no”. Laguna answered Waterway, survey jury west bank the Intracoastal also found that the Shine undisputedly boundary above that After this accurately level. marked commenced, the and failed to find litigation property Foundation com- Foundation’s Claunch/Lothrop so. Af- line did oceanologist, Dr. Reinhard missioned 3320, 5, 1995) (May Reg. Reg. (May 10. 20 Tex. 3320-3321 20 Tex. 3320-3321 1995) (proposing to amendment to 31 Tex. Admin. Code Tex. (proposing amendment Admin. 13, 1995) § 7.2); (June 7.2); (June 13, 1995) (adopting id. id. § at 4349 Code amendment). amendment). proposed (adopting proposed verdict, ter the the trial court issued parties’ arguments two application about its opinions explaining that while he had come their dispute.
to believe that the Foundation’s claims Humble, precluded
were though even A he had denied the State’s motion for sum- J.W. Luttes successfully peti- mary judgment urging preclusion, he tioned the Legislature to him to allow sue judgment would render on the verdict for 3,400 the State to determine title to some the State. acres of mud flats Madre on The court of appeals affirmed.11 In es- the east property side his in Cameron sence, the court concluded that Luttes does County,13 forty about miles south of the not preclude a determination of shoreline property Foundation’s the present boundaries without reference to water lev- predecessor’s case.14 His original 1829 els, evidence, and that there was historic grant, Vista, known as Potrero de Buena current, and support jury’s finding westerly was to the “shore” of the that the Shine line was accurate. Madre.15 Luttes contended that while the granted We the Foundation’s petition boundary originally shoreline had and for for review.12 In briefing, extensive many years beyond been a bluff which the parties have raised principal two issues: mud flats were then completely sub- here, whether and how Luttes applies merged, more recently the area to the east whether the Foundation’s claim preclud- had risen elevation because accretion ed Humble. We turn first to Luttes. deposits
due to of silt years, over the therefore he was entitled to the additional II property.16 The trial court made two im- The Foundation agree and the State determinations, portant one lawof and one that the result in the present depends case fact. The court concluded as a matter heavily on how we read our decision of law that under applicable civil law of they have accordingly focused Mexico, Luttes’s shoreline ended their They attentions on this vigor- issue. *7 highest at the level water reached. ever ously disagree over whether Luttes was fact, The court found aas matter of after a decided, correctly whether it applies, and trial, bench proved that Luttes had not what it means. In fairness to all of these elevation in the area was due to arguments, explain we first our under- accretion. appeal, On complained standing of Luttes with a far excur- more that the trial court had misconstrued the sive recitation of its text than we would civil law and that its failure find ordinarily so that accre- use what we think is its import against great pre- clear will tion was the and emerge weight from the words themselves. Then we will examine the of the ponderance evidence.17 The court of 1999). 11. 994 S.W.2d (Tex.App.-Austin 285 Id. at 169. (Jan. 13, 2000). Sup.Ct.
12. 43 Tex.
J. 301-302
Id.
357,
(Tex.App.-Waco
13. 289 S.W.2d
357
357,
1956),
remanded,
(Tex.App.-Waco
17. 289 S.W.2d
374-375
rev’d and
159 Tex.
324
remand,
1956),
remanded,
(1958),
S.W.2d 167
on
328 S.W.2d
rev’d and
159 Tex.
1959, writ).
(1958),
remand,
(Tex.App.-Waco
no
S.W.2d 167
328 S.W.2d
1959, writ).
(Tex.App.-Waco
no
14. See 159 Tex.
about 0.50 feet above the level of “mean court, by the trial and admit- found As high tide”. suit, is in parties ted there flats,] relatively vegetation no Madre little
[On there is sense, although are except which not have the true there algae, does frequent, appearance undoubtedly substantial vegetation normal levels irregular, forms sort of thin darkish mat over the variations water surface, up day longer period due to drying cracking during each *8 are the influence of non-astronomieal forces frequent periods when the flats free conditions, in and combina- of water.... The soil of the flats is sometimes in evidently a muddier tion astronomical tide conditions ap- of darker and with of of Mexico. One the factors pearance and character than sand Gulf to, substantially contributing causing, which and of or comprises flats beaches general in the area across the water levels Padre Island several miles northerly in of winds presence At least suit is the Laguna to the eastward. when Fall water, heavy period early Spring, to fairly the area is free of Id. Mat 187, 191. 19. 159 Tex. 324 S.W.2d at hand,
although, ano, on the other there quier tiempo have el en del inuierno o been recent instances of sea water over- del verano.”23 running the flats midsummer. There surveying the in- After several different present, is also at and due in least some of terpretations passage this over the cen- forces, part to a progres- astronomical noting expert testimony turies and of- sive, years slow rise over of fered Luttes and the on its State (“mean”) general sea level at an average we meaning, reasoned that both the Parti- rate of about 0.02 feet per year.21 das and common sense contemplated was, where shoreline water on the aver- Against began: the Court backdrop, age: granted We error largely the writ of Now whether the language confínes hope of being able eliminate the shore to that area regularly covered confusion that appears to exist at the and uncovered “tide” in the astro- what, Bar and otherwise as to details permits nomical sense or it to be practical application of cases like “swell”, highest may wave or rise that present, is the correct definition of the occur at this or that one hour particular being obviously shore—the matter one or minute from whatever other force public of considerable importance. We conditions, than “in all phrase, storm accordingly shall question discuss that (en año), year” undoubtedly todo el first. question leaves a year to what We harbor no the Mexican doubt that meant. Does mean the last calendar law, be, (Spanish) may whatever it year expiring before litigation at effect the date of grant, what other effort to fix the boundary on rule, must applicable furnish the ground, year or some earlier with decision, such every is the effect of level, higher water or the kind of aver- observation or assumption has ever age single highest of annual over levels made been this Court the sub- years, several on which the trial court ... ject. case, alternatively relied the instant Turning body we of civil stated: it mean daily or does that where the shore], The basic definition of [of highest levels over a are period years course, is body that of the celebrated evidence, of record and in hun- these law Spanish known as Las Siete Parti- highest dreds or thousands of levels das, which was evidently written averaged, average should be and the century 13th and promulgated some taken grows “however most it later, three centuries of which the yeaP’1! all the portion critical Title Partida Pretermitting for the moment . (from4 Lopez Law the so-called edition interpretive matter of we authority, at published govern- time under think language partidas Salamanca) auspices mental reads as sug- itself permits, common sense follows: gests, line based on a long term aver- “ ** * aquel daily levels, e todo es llamado lugar age highest rather *9 ribera de la mar se quanto theory cubre el than a line based on some of della, agua quanto sporadic mas crece en todo or highest occasional waters. Id. at 173. 23. Id. at 177. Id. at 175-176. the lower Indeed, disregarding year, us be consis- latest appears such to to arguments preceding of the levels of all the primary tent with one “highest” that the itself to the effect kind of the State if we are to use some And years. should, line should be one evidenced true “mean”, what evidently as we of the permanent markings on more or less in the words principle, in or is there ordinarily kind associated ground of the itself, an require such law the basic line upper the of a shore. Whatev- with highest an- single be that of average to in- aspect the the ground er the for of the several readings nual each case, is ordinarily a “shore line” stant one of question, rather than years and fre- regular characteristic of one readings days for all of daily highest sea, in turn quent coverage which averages are years? Both of such closely to an aver- much more related is only differ- readings. The highest water one, than to age daily highest waters highest read- lies in number of ence few, highest average merely a or averaged.24 ings readings. annual on a might be trivial That difference word, obviously “average”, While to the sea and astro- exposed open shore “mean”, not oc- equivalent, or its does the mean tidal forces. There cur, nomic suggested by language are both whole, vary much judge likely level is not as the trial water learned weekly, daily, are evidently recognized. particular readings No taken whether from which year being indicated as that to the monthly. But the difference due highest water “in all the so-called tide or can are taken readings over which interval taken, to be inference is year” in an area like be substantial prevailing a condition regularly days for dry Madre which is inundated a number of is what was years over at a days several the water at a time. For intended, suggests and this in turn on while spot may deep, foot given If, for period. mean taken over such a dry. To days place completely other single water for example, highest annual highest locate the shoreline years immediately five prior each of the level in this water area litigation to the were no instance reasoned, we would higher than one above mean sea foot present no the time was most of level, to be but were somehow shown all. there at long particular year three feet one line, we base the as did Thus should years, to the latest it would prior five levels, court, exceptional these few in- hardly appear within the reasonable of shore likely to have a line we are for- tendment of law that we should commonly ac- not shore which is years later fix the line at get the covered being regularly sense of cepted one more according three feet It is difficult and uncovered water. Conversely single if the year. remote writers of that the ancient to believe just preced- reading year highest which had mind a shore paHidas feet, those the trial were while ing two accepted commonly from the different years preceding of nine or for each more more thinks of shore thereof. One foot, idea were not one the latest over edge than in terms of water’s fix- require would seem unreasonable occasionally land which is at the terms of ing the line two-foot level Id. at 179. *10 irregularly highest inundated.25 water levels is use of the (water)”. high standard of “mean tide But how to obtain the water level data delay year, While this involves a of a averaged to be when gauges, though tidal appears practical waiting it more than coast, along scattered the Texas were of- years get several an average order to apart? ten far way One would tobe ob- single highest of annual waters over the tain evidence from sources less rehable event, longer period. In either the local than gauges. tidal Another would be to because, tide gauge necessary as stat- abandon the high water level mea- ed, vary considerably water levels surement altogether simply rely on place place Laguna, particular- to eyewitness testimony to high establish wa- ly varying exposures on account of to Instead, ter rejected levels. We both.26 forces, whereas, meteorological we explained: (water)” adopting the “mean high tide standard, period gauge oper- of tide A third and much more reliable alter- may year.27 ation reduced one native, be however, following is that of system (water)”, high of “mean tide
which effect is average but the of average, Once we elect for an as the highest day water of each rather than practicalities require, seem to and the each If year. adopted, that rule is we texts of neither the Roman Law Civil have, by can installing gauge a tide for forbid, partidas appear nor the year little as one near the area in average sounder course is to take the question, highest the benefit of 365 read- daily gauge readings daily high- tide ings upon average, which to base an water, est tide or a wind-driven is, upon which to determine high “mean wave.28 (water)” tide point at that for that one year. This mean obviously level will rejected highest We water level rule vary corresponding less from a level for being announced in Humble as an incor- (or later) years earlier than would a interpretation rect of the civil and we single highest year annual level for one nothing found the law of other states to vary from respective highest annual reading contradict our of the Partidas. Indeed, years. levels of Finally, rejected argument other as before we stated, upon quite fixing daily the further and sim- at shore the level of mean ple step high of correction unfair against the nearest water was to the State and gauge importance actually tide which instead operation has been stressed ascertaining opposed for water levels as 19-year cycle, the full tidal the one- (water)” relying testimony litigation. adduced for year figure “mean high tide gauge the local will reflect with reason- Theoretically, high the rule of ably close exactness the “mean tide is less to the State its favorable (water)” 19-year cycle. for the whole than a rule capacity as landowner words, other far single highest so as most Texas on a instance of based concerned, way coast is reliable annual or a mean of several such average which to obtain sort of instances. But that is not reason 25. Id. at 180. Id. 181. added). (emphasis Id. Id. at 182 *11 retreat our conclusion than not differently law but we did interpreting
our placed law the shoreline were that the civil only private if interests we would level, rejected the specifically and we Moreover, far from that are involved. we be locat- that the shoreline could rule of argument that in actual practice sure line, had which we a an “obvious” bluff is than ed at high mean water less favorable very really obvi- already remarked calling for a line that higher rule shore of ous. always vague be and difficult will on the finally until fixed
ascertainment to that may be the case as Whatever complicated after ground extended and An- by the governed shores part of our A result latter kind of litigation. tide, we high rule of mean glo-American abutting well be may give rule to say Span- it to that the do think correct (and landowner his mineral les- private (Mexican) law the shore is concept of ish see) advantage an in the over the State cov- regularly in which land the area is litigation, he has inevitable because a by uncovered the sea over ered and kind of longer and better access to the If a given it be long period. shown proof necessarily that will be involved shore, as upper level case that of demonstrating such and whether on by actually covered uncovered year such an occasion and such a such (or lower) sea, higher than the level years one or waves” “highest more high by determined higher tide as actually irregular reached or that appears and if it gauges, tide also may ground. line on the Another result shore, upper median line of discourage leasing be to mineral regularly and uncov- actually so covered by tidal areas from smaller the State ered, can be determined with reasonable operators who cannot run the risk of by exclusive re- accuracy otherwise than complicated boundary litigation addi- gauges, do not our sort to tide we explo- to other tion risks of mineral a case. intend to foreclose such opinion ration.29 case, quite plain instant to In the analysis Concluding our we regularly of the civil that the area suit is not us “that specifically held rule of applicable covered and uncovered (Spanish) determining long Mexican has not time. [in law waters and been for exists, highest merely that of there average say shoreline] is To because edge, line” or daily computed water over or corrected at the western a “bluff line”, cycle regular years.”30 marking tidal of 18.6 where “vegetation mis- appeals’ period court of at some Concerned waters undisclosed interpretation might evidently regularity, the civil law did reach with taken past its of the evi- line is the line of mean have influenced assessment the latter would, accretion, tide, case in our be much opinion, dence of we remanded the light than fix a fine of mean sufficiency for a factual review less reasonable rule of tide exclusive resort the announced law.31 gauges.32 rehearing, acknowledged we that a On we had any dispute de- over what daily high might level To eliminate rule for to be civil law gauges, termined otherwise than tidal determined Id. at 191. Id. at 186-187. 31. Id. at 192. Id. at 187. *12 shorelines, determining the dissent articu- under the civil law. It is not limited rejected: lated what the Court had facts Mr. Luttes’s case. As the Court granted large- said: “We the writ of The shoreline should be determined ac- error ly in cording hope being to the civil law. This line can- able to eliminate not, circumstances, under appears be accu- the confusion that at the exist rately by what, determined the use of the tide Bar and otherwise as to details of gauge. According to provisions of practical application pres- to cases like the Partidas, Las Siete the seashore is the ent, is the correct definition of the shore— land is covered with water from being obviously the matter one of consider- Spanish time to time. The verb “cubrir” able public importance.”35 used, is which means “to cover”. The general Second: conditions seashore, then, portion is that is property Madre east of Luttes’s alternately covered uncovered the 1950’s are no different those east height the sea. The of the water on the now, of the Foundation’s property only gauge height is not the same as the forty away: miles seawater inundation is of the water that or up up rolls is blown shallow, regular, infrequent, and somewhat on the gauge might shore. The tide be mostly by and it is caused seasonal meteo- prima used to facie the location establish rological forces but nevertheless affected shoreline, always but should be slightly by daily astronomic forces. prima held to be facie evidence of the true line. Such evi- presumptive boundary original Third: The may destroyed by dence be the facts. grants civil law must be determined words, question other of the loca- law, subsequent surveys not or the tion of shoreline is one of fact and grantees conduct of the or their succes nothing one law. There is sors. dealing Partidas definition with tide gauge.... gauge The tide A boundary would Fourth: shoreline can wholly inaccurate to establish the true not be determined without water level measurements, seashore line.33 gauges even if no tidal historically placed adjacent
have
been
property, and even if
measurements
those
It seems to be unassailable that the
are made for no reason
to determine a
contemplated
civil
year.
[“shore” mean]
law
over as short a time as a
sea,
actually
the area
reached
An historic
line
not mark a civil
bluff
does
though only
single
swell. If the tide
boundary.
law
gauge
accepted as the absolute deter-
level
relevant
Fifth:
locating
minate
the shore-
placing
highest
measurement
is not the
level that
line, then we are
a rather
establishing
water ever
but a mean level.
reaches
artificial line.34
Luttes,
following propositions
From
calcu
Sixth: The mean should be
may fairly be said to be established:
basis,
if
daily
daily
lated on a
even
to,
does,
atmo
purports
change
First: Luttes
water levels caused
generally
spheric
very
tidal forces
small.
determine shoreline boundaries
J.,
(Smith,
dissenting).
Id. at 196-197
35.Id.
at 175-176.
J.,
(Smith,
dissenting).
Id. at 197
on the civil
array of scholars
formidable
understanding
This is our
although in reference was
parties’ arguments
with it we turn to
expert testi-
by the kind of
texts unaided
ease.
But
present
case.
mony adduced
now
argument
in the record and
nothing
B
*13
re-
us that we should
before us convinces
arguments.
consider first the State’s
We
in Luttes.
determined
the rule
consider
in this case
contrary,
the record
On the
1
uncertainty
apparent
even more
makes
argues that Luttes miscon-
The State
Partidas;
the State’s
interpreting
in
strued the Partidas.
interpret-
Properly
for a different
arguments
evidence
ed,
says,
placed
the civil law
the State
Foun-
so are the
persuasive,
rule are
levels
highest
water
shorelines
arguments for the
dation’s evidence
storms,
ordinary
not at mean
reached in
rule of Luttes.
simply impossible
It is
tells us
daily high water levels. The State
eighteenth-century
how
know for certain
proper
that while
construction
“[t]he
their
applied
Mexico would have
Spain and
Partidas was
extensively
by
briefed
[the
]
determining
law for
thirteenth-century
of the best
parties
some
difficult context of
shorelines
state”, the
in this
lawyers
practicing
then
Laguna Madre.
subject was lim-
evidentiary record on the
civil
interpretation of the
The Court’s
case,
says,
ited.
In this
the State
workable,
law Luttes is
reasonable and
retained some of the fore-
parties
determining
rule
provided a
and it has
Spanish
on ancient
law
experts
most
forty years.
than
for more
boundaries
reports
proper
their own
on the
give
subject is not
recognize that the
we
While
of the Partidas:
Professor
construction
reconsideration,
stare decisis
beyond
Litvinoff, of Louisiana State Uni-
Saul
land ti-
protecting
than in
stronger
never
Luis
versity, and Professor Jose
Sober-
virtue in
tles,
great
there is
as to which
Fernandez,
Na-
anes
of the Universidad
very
reluctant
certainty.36 We would
Mexico, for the
cional Autonoma de
determining
rule
seashore
discard a
State,
Hans Baade and
and Professors
long
that has served
boundaries
Margadant,
Guillermo F.
both
Luttes, thereby
the rule
satisfactorily as
Texas,
University of
for the Petitioners.
and we
expectations,
long-settled
upsetting
evidence,
argues,
the State
Based on this
compelling
far more
not do so absent
could
reexamine Luttes n
inter-
Court should
can be offered here.
evidence than
of the civillaw.
pretation
we
reaffirm
Accordingly,
premises.
accept
We
all of the State’s
land
in civil law
boundaries
shoreline
in fact
meaning
of the civil law was
with reference
grants must be determined
briefed in Luttes
some
extensively
levels.
daily high
to measured
Texas,
lawyers in
and we hasten
the best
subject
given
been
to add that the
has
2
thorough
pres-
treatment
even more
rule of Luttes
argues that the
The State
lawyers every
equals
bit the
ent case
is claimed
the shoreline
only when
counsel in Luttes.
applies
cases the Court
both
of accre-
over time because
truly
to have moved
of a
has had benefit of
views
Wilkinson,
Aviation, Inc.,
70
234 S.W.
Mustang
111 Tex.
v.
36. Marmon
(1921).
(Tex.1968);
v.
Cross
n.
S.W.2d
true,
course,
tion or reliction.
It is
Spain
that The intent of
granting
and Mexico in
Luttes himself
land to
predecessors
made such a claim.
It
the Foundation’s
true, however,
must be
not
determined
reference to those
that the civil law deter-
sovereigns’ policies and laws at the time of
mined any way
dependent
course,
grants.39
survey
A
may, of
on the occurrence of accretion or reliction.
intent,40
give
grantor’s
some indication of a
What Luttes established was nothing less
grant
but when the
calls for a natural
applicable
than “the
rule of Mexican
boundary here,
monument as a
“the wa-
(Spanish) law” for
—
determining seashore
ters of the Laguna Madre” —that monu-
An interpretation
boundaries.37
of the civ-
ment controls over courses and distances
held,
il
we
was necessary to under-
by survey.41
determined
Generally, a sur-
accretion,
standing Luttes’s claim of
veyor’s meander
along
lines
a water line
vice versa. The rule of Luttes applies
*14
do not
boundary.42
mark the
We have
whenever a civil
law shoreline
determined-what
Spain
the intent of
and
in question.
law,
Mexico
by interpreting
their
Partidas,
Luttes. That their
grantees
3
surveyors may
have had a different
be,
been,
understanding must
and has
con-
argues
The State next
that the rule
sidered in interpreting the civil law.
In
Luttes should not be
of
applied
in this case
words,
interpretation
other
of control-
because
result
contrary
its
to the sur
ling eighteenth century civil law must take
veys
grants
of the
at the
they
time
were
into account how it
was understood
afterward,
century
made and for a
and to
time,
those who
applied
including
at the
understanding
uniform
of the Founda
the original grantees and
surveyors
predecessors
tion’s
in interest until at most
property at issue here and those who suc-
past
reasons,
few decades. For two
ceeded them. But having determined
we do not agree.
was,
what the applicable civil law
as we
Luttes,
have in
taking
after
all such consid-
First,
firmly
it is
established that
account,
erations into
we cannot then re-
rules for the
grants,
[t]he
construction of
application
fuse its
happens
where there
boundaries,
and for ascertaining their
be
particular grantees
evidence that
which have from time to time been an-
surveyors
understanding
had a different
nounced
the court and have been
misunderstanding
law. Their
of the
lines,
acted on in establishing their
are
applicable
grant-
law cannot diminish the
all
for
designed
purpose
carrying
grants any
ors’
more than it
enlarge
could
out the intention
grantor.
of the
When
them. The civil law does not locate “the
manifest,
this intention is once made
all
place
waters of the
Madre” at one
yield
else must
to and
governed by
be
any contrary
when there is no
evidence
it.38
smweyors
understanding by owners and
Luttes,
500,
Frandolig,
159 Tex.
preted
sum,
bound-
Foundation’s eastern
understanding.
regard
private
Madre”-—
of the
ary
waters
—“the
law in effect when
the civil
is fixed
Second,
ambigu-
the historical record is
can neither
made and
original grants were
of the different motives
ous because
parties’
reduced
enlarged nor
be
v.
noted in State
actors over time. We
at that time
misunderstanding of that law
Island,
Balli,
the title to Padre
regarding
course,
not,
a case
This is
or since.
often made to determine
surveys
were
to have aban-
is claimed
which an owner
paid
sovereign
what dues were to
challenger
in which a
property or
doned
rather
grazing
land was usable for
what
is a case
possession;
claims adverse
pur-
boundaries for title
than to ascertain
a natural monument
construing a call for
grant-
the first
poses.43 Unquestionably,
The relevance
original grant.
in an
land suitable for
principal
ees’
concern was
is in
by the State
historic record offered
petition
That
Balli’s
grazing.
explains
law.
determining
applicable
Once
adjacent
Big
Bar-
Rincon
Mesquite
however,
determined,
as it
law has been
adjustment to the
reta and de la Fuente’s
en-
it can neither be
has been
Little Barreta. Both were
survey of the
diminished
under-
by private
larged nor
*15
grazing
possessed
that the owners
ensure
standing.
argues that because the
land. The State
4
Mesquite
wholly
Rincon lies
within
in
if Balli owned it
dispute,
area now
rule deter-
argues that the
The State
as the Foundation
grants,
virtue of his
or sensi-
practically
in Luttes cannot
mined
it;
claims,
for
petition
he had no need to
Laguna
of the
bly
in the area
applied
in
it must not have been included
therefore
property
the Foundation’s
Madre east of
any
area
grants any
more than
other
there. As
of the conditions
because
of the bluff line.
Balli’s
east
Whatever
out,
jury found that
points
State
may
petition—
intent
have
his
been
could not be determined
higher high tide
Rincon
acquire
Mesquite
whether to
But it is
accuracy there.
with reasonable
own, merely
he
or
to confirm
Luttes,
did
as well as
opinion in
plain from our
in
grazing
land
an area he
ownership
his
fact in
findings of
from the trial court’s
already
grazing
where
was for
owned
in the court of
extensively recited
that case
regard
impossible
cannot
part
only apprecia-
most
opinion,44that the
appeals’
—we
limiting
Spanish grant.
at the
Laguna
his intent as
in the
Madre
ble difference
or
sovereign’s
“always”
in-
water
Nor can we determine the
is that
two locations
the area east
“completely”
for the
covered
granting
petition
tent
in
Balli’s
inundation east
Rincon,
while
property45
Luttes’s
Mesquite
apart
govern-
thereafter,
195,
Balli,
century
the area in suit
over half a
rise in elevation—and a
water level measurements should not be
But
made the
tion and terrain.
the State
used to determine
“shoreline”
Luttes. The evi-
argument
identical
adjacent
Madre
the Foundation’s
is that water
present
dence
case
property because such measurements are
reaches the bluff line at most once or twice
after
meaningless
so difficult and
The evidence in Luttes was com-
year.
Atmospheric
Ad-
the National Oceanic
parable.
days
Evidence of the number
any
to make
ministration abandoned
effort
flats,
inundation of the mud
even
them. But the civil law rule determined
line,
comparable
east of
bluff
also
*16
Luttes
predated
predeces-
and its
NOAA
Daily
forces
both cases.46
astronomic
sor,
the
States Coast
Geodetic
United
in
Madre
stronger
Laguna
were no
the
the
Survey, by
century,
more than a
they
than
are near
property
near Luttes’s
in Luttes
in
Survey
was mentioned
the
There were no
property.
Foundation’s
of passing. Application of the rule
vicinity
immediate
gauges
tidal
policies
or its
dependent
is not
on NOAA
just
there are none
property,
Luttes’s
as
gauges,
nearby
or the
installation of tidal
property.
near the Foundation’s
Luttes)47
(as
private
whether
one was
that under
condi-
argues
The State
such
governmental.
tions,
regular
inundation is
but shal-
when
argues
impossibility
The State
that
it makes no more
infrequent,
low and
daily high water levels
measuring
presence
of water
sense to determine
Madre
demonstrated
Laguna
is
measured on a
using mean water levels
and its
efforts to do so
the Foundation’s
daily
than it does to describe the
basis
in this
it has taken
position
to the
retreat
by saying that
Corpus
climate of
Christi
level is not a
applicable
that the
litigation
72°F. But
daily temperature
its mean
is
arbitrary
one—one
measured one but
argument
made this same
State
Luttes,
Vertical
above the
Geodetic
rejected it there.
foot
National
expressly
and we
any
than
1929—that is
Datum of
sense to determine a shore-
It makes less
conve-
be measured and which
level
ever
that could
highest
line based on the
water
Luttes,
ary rarely at a bluff water reached: Ill case, quite plain
In the
it is
instant
regularly
area in
is not
argues
us
suit
that the Founda
The State also
covered and uncovered
claims in this case are barred
res
tion’s
long
a
time.
estoppel
waters and has not been for
judicata
and collateral
—often
exists,
to,
merely
there
say
usefully
respectively,
To
because
as
more
referred
edge,
at the
a “bluff line” or a
preclusion—
western
claim
and issue
preclusion
line”,
“vegetation
marking where the
findings
trial court’s
based
the federal
in the
period
waters at some undisclosed
in Humble
holdings
and the Fifth Circuit’s
Co.,
evidently
regularity,
with
past
did reach
decided
Refining
&
Co. v. Sun Oil
Oil
Humble,
line is
line of mean
already
the latter
as we have
in 1951.50
tide, would,
said,
Oil,
be much
opinion,
our
mineral lessee
Sun
State’s
to fix line of mean
less reasonable than
at issue
part
of the mud flats
case,
tide
exclusive resort
prede
the Foundation’s
present
sued
gauges.49
and their mineral les
cessors
interest
see,
Oil, to determine whose lease
Humble
boundary
urges
The bluff line
the State
permitted
court
was valid.
district
present
indistinguishable
case is
litigation
to intervene
State
urged
the bluff line
the land at
competing
owner to title to
foreclosed
argument
and its
is therefore
issue,51
the Fifth Circuit reversed
our decision in that case.
presence
of the State as
ruling because
C
diversity jurisdiction
party
would defeat
Fifth
on which the case was based.52
rejected
arguments
the State’s
Having
could
trial court
“[t]he
in this Circuit held
regarding
application
of Luttes
jurisdiction over
case,
acquire
not and did not
briefly
turn
to the Foundation’s
we
*18
establishes,
of Tex
controversy
between the State
and
position. The evidence
Co.,
Refining
Oil &
51. Sun Oil Co. v. Humble
Id.
49.
(S.D.Tex.1950).
F.Supp.
88
658
Co.,
Refining
v.
Oil &
50. Sun Oil Co. Humble
(S.D.Tex.1950),
and
F.Supp.
88
658
modified
Humble,
F.2d at 197-198.
52.
190
Refining
Oil &
Co. v.
sub nom. Humble
aff'd
Co.,
(5th Cir.), reh’g
Sun Oil
288 fully fairly liti- second action were purpose.”62
for that (2) action; in the first those facts gated rule, liti Under this the Humble in judgment were essential gation preclude does not the Foundation’s (3) action; parties were first in case. The federal present claims in cast as adversaries the first action.65 court in Humble did not determine district just explained, For the reason we have boundary the eastern of the Foundation’s concerning facts Foundation’s eastern property and could not have done so. Not fully fairly litigated not were all of the area was involved in the case. Only a in the Humble case. fraction of the in over the parties’s dispute The Humble area on the east side of the Foundation’s cov validity competing mineral leases dispute property was issue. The central of the area part ered a small boundary in the was not over the civil law Oil, present case. dispute Sun there had original grants but over whether lessee, did not claim an interest State’s intervening years. accretion in the been along most of the land the east side of the property, Foundation’s and therefore could in land importance stability The State, litigate boundary. not that moves us to adhere to the rule titles said, party we have was not Humble require stated in Luttes does not we its have defeat because intervention would litigation preclusive effect give the Humble diversity jurisdiction on which the ac ed regarding in this case. The facts reason, predicated.63 tion was For this boundary were not deter Foundation’s litigation pre Humble cannot be held to mined in Humble and could not have been. present clude the claims made case. interpretation federal courts’ original grants is governing civil law estop- for whether collateral As us, rejected and we binding preclusive effect of the federal pel—the of law are not Luttes. Determinations present litigation case on of issues effect.66 generally given preclusive state governed by case—is federal or previously we have concluded both Furthermore, the Humble case give are the same.64 Under both federal and not serve the preclusive effect here would Texas law: principles preclusion serves.67 Shore, v. the United seeking Hosiery
A
the bar of Parklane
Co.
party
to assert
judi-
stated that res
estoppel
Supreme
must
States
Court
collateral
establish
(1)
“the
estoppel
cata
both serve
sought
litigated
the facts
to be
and collateral
Sunnen,
591,
Servs.,
Sysco
Trapnell,
65.
Food
Inc. v.
890
62.
v.
333 U.S.
Commissioner
597,
715,
(1948)
796,
(Tex.1994)
(quot-
(citing
898
v.
68 S.Ct.
92 L.Ed.
801
Allen
S.W.2d
Sac,
(4
411,
ing
County
90, 94-95,
v.
94 U.S.
Cromwell
McCurry,
S.Ct.
449 U.S.
101
accord,
351, 352,
Otto)
(1876));
Quaker
289 Y litigants from protecting purpose dual an identical issue relitigating the burden of response word in Finally, we add a brief n withthe same his and of party privy to the dissent. economy by judicial preventing promoting is that argument principal The dissent’s to Even if we were litigation.”68 needless Laguna in the assumes that part to that Humble determined title hold measured, “that as- Madre can be in it could not dispute, of the area now longer viable because we is no sumption litigation over the remainder preclude that, as con- undisputed fact now have the area. tide, government, the cluded the federal Madre, Laguna in part at least conclude that the Humble We therefore trying to measured.”72 Without cannot be litigation of the title preclude case does not it, actually on what we put point too fine a present case. issues involved government federal know from the 1995, thirty-seven years after Luttes IY present after this shortly was decided and the National Oceanic litigation began, address is The last issue we must Administration, a bureau of Atmospheric to re whether the Foundation is entitled Commerce, issued Department the U.S. basis the attorney cover its fees. cooperation with developed a report recovery is the Foundation claims for such Office, party Land to Texas General Act, Judgments autho Declaratory which concluded, case, for which present rizes an award of reasonable and neces and not navigation of commercial purposes just sary attorney equitab fees when titles, regions land determining attorney fees to be le.69 We allowed Madre, the area ad- Laguna including against awarded the State in Texas Edu “should jacent property the Foundation’s v. involved Agency Leeper,70 cation which da- ... non-tidal for tidal be classified as enactments, and challenge legislative op- according computation purposes tum argues that also the Foundation we should Na- [the criteria established erational dispute award fees here. But the for tabulation Service] tional Ocean title, over not an enact present case is too forces atmospheric tide”73 because ment, and the Foundation’s claim for de region for levels in the affect water greatly claratory merely relief is incidental to tides to be measured. astronomic circumstances, In such title issues. changes in any not on report was based of attor Act does not authorize an award Madre —no one conditions Moreover, the ney against fees the State. changes have been contends that there Natural Code provisions of the Resources prop- Foundation’s region near the permit which the Foundation sue on what years hundred erty two —but for recov in a series of provide says in this case do not is “the latest report State tidal char- understand the efforts to NOS ery attorney fees.71 322, 645, §§ 33.171-.176. 58 71. See 68. U.S. 99 S.Ct. Tex. Res.Code Nat. (1979). L.Ed.2d 552 72. Post § 37.009. Civ. Prac. & Rem.Code Atmospheric Admin- Oceanic and Tex. 73. National istration, and Datums of Characteristics Tidal 1995). (July (Tex. 1994). Texas S.W.2d *21 many years, Texas”.74 “tidal” as it did for or to call acteristics of in were them “non-tidal” as it its 1995 re- governing report criteria has in early port, high nineteenth cen- water levels can be measured provisions not just they as could be tury Spanish disputed and Mexican civil law but area Luttes, daily in and measure- policies. purpose recent NOS of the measured mean, get report averaged was not to fix land titles but to ments can be adjusted tabulations. that mean can be with actual and guide NOAA’s tide Yet argues report, extrapolated epoch that this written data over tidal of 18.6 dissent cooperation years. oceanologist in The Foundation’s did litigation began, after this using daily high different that and determined that mean parties, with one above the criteria than those which determine this water was 0.60 to 0.75 foot supersedes disputed NGVD over the area. There is purposes case and for different area, present regular disputed Luttes and the civil law. Had the flow of water open before the but not like an beach. Water flow is litigation report been concluded issued, report regular places peri- or had the been withdrawn both over different concluded, might litigation before this the dis- ods of time. NOAA the dissent “tidal”, consider flow their senting presumably Justices would favor not understandings do not fix the Foundation’s position. the Foundation’s The dissent’s early century boundary. that nineteenth The civil law does. The issue position is case, rhetoric, stripped obscuring Spanish and Mexican civil law and Texas movement of water along regular land the seashore fluctuate de- is whether the titles it a disputed over the area makes “shore” pending evolving on NOAA’s understand- original land ings region. meaning of tidal characteristics within the at the grants governing federal has de- and the civil law government “[t]he Because as in Luttes. That de- clared as a matter of law the tide time construed measured,”75 Luttes according pends cannot be to the on whether the conditions dissent, materially considered different regarding the civil law shorelines were case, to that from 1804 to those in this and the answer applied grants to these land 35,000 no, we have shifting passages 1995 and then as the extensive stopped, quoted from Luttes demonstrate. acres from the Foundation State. great respect power With for the using dai- argues The dissent agree we do not government, federal to mark the shoreline ly high water levels can agency’s understanding of nature junk simply in an area like this “is sci- history. alter But the of where ence.” determination a matter of Madre in to mark a shoreline is The conditions the shore- might place are science. The law region present involved case by water highest in line at the level reached region the same as those in the involved annually, example the court the Foundation has mea- Luttes. What the civil law did. has called Humble Oil concluded sured —what NOAA sometimes at might not—is the Or the law locate shorelines precisely “tide” and sometimes elevation, as the changes vegetation daily high water level fact, here. argues should be done says requires the civil law to be measured. State however, according eighteenth call such levels Whether NOAA chooses to 76. Post Id. at 53. at-. Post ex- grantee could either surveyor No neither but instead century civil law did daily high meaning of the sover- where mean or contract the pand marked shorelines *22 upland. water intersected levels eign’s grant. of policy based on the civil law rule was studiously ignores Finally, the dissent served, “junk it science”.
the cultures not reach- that water fact: very important one years hundred later reject that rule two To as a line the State claims the bluff es un- thinks it was because this Court now a It year. at most once or twice boundary junk The dissent sound would be law. place of a shore as the is odd to think argues that Luttes was adopt ill-advised to never is. where water almost circumstances, all but single a rule for Luttes inter- rule; Luttes did not adopt a Spain that and Mexico had
preted the rule we explained, we have For the reasons that rule was well—or adopted. Whether ap- judgment of the court reverse grants irrelevant. The ill-considered is the case to the trial peals and remand and in Luttes are by governed this ease judgment in accor- court for rendition rule, was, law whatever it the civil opinion. dance with this it Luttes expressly determined what was. boundary suggests The dissent that the dissenting filed a Justice ENOCH high a mean wa- using line determined BAKER in which Justice opinion,
ter
level one foot above the NGVD is
joined.
Justice HANKINSON
boundary
different from the
be
would
using
determined
actual water
mea-
level
dissenting
Justice ENOCH filed a
surements,
simply
but
this is
not true.
BAKER and
opinion, which Justice
high
is
as
Whether
water
as low
joined.
Justice HANKINSON
seven inches or as
as twelve inches
v.
Luttes
decided as a matter of
State1
NGVD,
above the
line is
boundary
Texas shorelines are measured
law that
exactly the same:
west bank
well,
high tide. As
the mean
Waterway.
Intracoastal
The evidence
Luttes answered is
decidedly
dif-
question
not,
not,
does
need
show where
in this case-—
question
ferent from the
boundary was
before
Intracoastal Wa-
fact the mean
whether as a matter of
terway
dredged.
was
can be measured. The
higher high tide
argues
The dissent
that historical evi-
Luttes, but
today
misreads
Court
dence better shows the location of the
Luttes’
question
of law with this
conflates
line,
though
even
it concedes
I
question
respectfully
of fact.
dis-
case’s
surveys
were not intended to establish
sent.
impor-
boundaries. Historical evidence is
case,
that, in
the tide
Clearly aware
tant in
the civil
trying to understand what
measured,
Court, ostensibly
cannot be
shoreline,
law meant
a
but once that
measuring high
relying
equates
it
interpreted,
law has been
cannot be
water levels
measuring daily
tide with
survey-
defeated
the views of individual
so,
by doing
But
the Court
Laguna.
ors and others. Luttes held that
what
strips Luttes
any legitimate
foundation.
they grant-
Spain and Mexico meant when
measuring daily
Luttes
did not decide that
daily high
ed land to a shoreline was mean
the same
levels in the
said,
water
That
the historical rec-
water level.
levels,
daily tide
thing
measuring
particular
longer
ord in a
case no
matters.
(Tex.1958).
1. 159 Tex.
rather it assumed that those water levels
dered
Bill
veyed by
Lothrop
All
Matt Claunch and
parties agree
reflected tide.
because that line is somewhere above
requires computing
levels
Hardly
jur-
tide line.
18.6-year period.
over an
What the Court
years
length
is the
sound decision. One would
ignores
isprudentially
18.6
Thus,
Luttes neces-
pressed
hard
to find
case
Texas
cycle.2
an entire tidal
court
being mea-
which the
awarded
sarily requires
jurisprudence
the water levels
here,
party
party
on what the
judgment
And
sured to be tidal levels.
willing
party proving
to take absent the
cannot be measured.
*23
something.
to take at least
was entitled
fault line
bridge
The Court tries to
this
Furthermore,
Claunch/Lothrop line
the
Luttes used
in
that the
noting
Court
purport
daily
does not
to locate the mean
the
when it concluded that
word “water”
level,
water
let alone the mean
higher high
La-
higher high
the mean
tide line
the
Rather,
a line
tide
it locates
one foot
line.
could be determined. And because
guna
Da-
above the National Geodetic Vertical
conditions here and in Luttes
Laguna’s
(Datum Plane), which is a
tum of 1929
same,
essentially
are
the Court accord-
adopted
geo-
fixed reference
as a standard
higher high tide
ingly concludes that mean
elevations determined
detic datum for
in this case as a matter
can be determined
leveling.3
bridge
law. But the Court’s
crumbles
litigation and even
parties
a fact the
assumed
All the
to this
the absence of
Court
can
mea-
knows that no one
deter-
in Luttes —that
the tide could be
Court
it
Luttes assumed
All
that mine the mean tide line and use
to locate
parties
sured.
margin.
west
And
some tidal movement could be measured.
Madre’s
course,
scientific co-
longer
ignores
is no
while the Court
this
assumption
Of
nundrum,
end,
obviously
it
con-
undisput-
now have
viable because we
that,
high water measurements cannot be
ed fact
concluded
the federal
cludes
tide,
legal
evidentiary
For with no
or
part
at least
used.
government,
instructs the trial court
support,
cannot be measured.
the Court
judgment
to enter
for the Foundation us-
finding
impossibility
To avoid the
Plane
one foot line.
ing
plus
the Datum
tide,
higher high
mean
the Court slides
Luttes
ignore
the rec-
really
But the Court need
asserting
into
that what
formula to non-tidal
apply
ord and
tidal
water level could be
meant
proper
18.6-year
cycle
tidal
data to determine
against the
measured
years of
have two hundred
mean. But
this case. We
the water levels’
to determine
margin
Lagu-
history about the west
junk science.
If one is not
simply
that is
establishing
tide,
us. And
guide
na Madre to
extrapolating
then
measuring the
evidence is
boundary using historical
you have
water measurement
whatever
by pre-Luttes case
law.
fully supported
18.6-year
cycle simply pro-
tidal
over the
Moreover,
produced
the State
evidence
produce
a number.
It doesn’t
duces
that the
jury finding
State’s
Regardless,
supporting
tide.
higher high
mean for
which was
on
boundary,
based
obviously
problem
proposed
be-
sees
Court
docu-
evidence and historical
judgment
any physical
on
cause rather than render
ments,
with rea-
margin
marks the west
line,
judgment
be ren-
it directs
Operational
See
Servs., U.S.
&
rehearing).
Ctr. For
Prods.
(opinion
Id. at 192
Glossary
Dep’t
Commerce, Tide and Current
(1999).
epoch,
tidal
18.6-year
to an
I would correlated
accuracy. Accordingly,
sonable
forces in the tidal
appeals’ judgment
court of
all the astronomic
affirm the
which
clear
of the State.
This intent
is also
cycle appear.6
favor
“tide,” quot-
definition of
from the Court’s
LUTTES
I. THE PROBLEM
WITH
above,
the predictable
focuses on
ed
which
Luttes, irre-
insisting
with
problem
on astro-
and fall of the waters based
rise
facts,
controls this case is
spective of
And it is clear from
nomic factors.
peg
forces a round
into
that the Court
States Su-
reliance on
United
Court’s
applies
the civil law.
square hole.
in Borax Consoli-
preme
reasoning
Court’s
using
law locates seashores
And the civil
Borax, dated v. Los
Angeles.7 In
Su-
The Court as-
tide.
approved the
expressly
Court
preme
sumes,
per-
that Luttes
when
concludes
methodology of the U.S. Coast
Geo-
merely high
mits
be measured
(a
today’s
Na-
Survey
precursor
detic
tide, that a mean can be
and not
Atmospheric
Adminis-
tional Oceanic
have for
calculated. But the formula we
NOAA)
tration,
calculating
*24
requires using
mean
the
calculating this
high tide.8
Thus,
18.6-year
cycle.
tidal
it is the tide
that water lev-
Although acknowledging
simply
and not
that must be measured
strongly
Madre are also
Laguna
els
the
water levels.
forces such
affected
non-astronomical
established,
As Luttes
grantors of
when
in Luttes
weather,
as wind and
the Court
civil-law littoral
tracts used the word
tide could still be
clearly assumed that the
“shore,” they intended that it be the area
fact,
so far
In
the Court went
measured.9
the
regularly covered
uncovered
that advancements
science
as to assume
time,
over a
that
the
long period
sea
tide even easi-
measuring
would make
the
shoreline,
level of the shore be the
upper
get to the answer
er.10 But science didn’t
and that
the shoreline be located at the
Since Luttes was de-
expected.
the Court
higher high
line of mean
tide.4
select-
cided,
that the tide
NOAA has concluded
mean
tide
ing
shoreline
Lagu-
in areas of the
cannot be measured
measurement,
the Luttes Court
explained
“
along
disputed
including
na
its
that
regular
predict-
‘tide’ means
margin. And the Foundation offered
(or rises)
west
perpendicular daily
able
rise
Rather,
(or falls)
no
otherwise.
evidence
fall
as a result of
waters
NOAA, publish-
report
evidence is a
forces, wit,
gravitation-
astronomical
to
1995,
analyzes
ed in
which
(mostly
al
of the sun and moon
pull
concludes
latter)
tide characteristics and
Madre’s
That the
upon
earth.”5
Court
accurately
that the mean tide cannot be
in Luttes intended the tide be measured is
property.11
along
disputed
calculated
specification
clear from
Court’s
NOAA,
acting
forces
According
be
other
daily
gauge
tide
measurements must
500,
500,
Luttes,
6. Id. at
Gill,
K.
James
Dingle,
Dept
Gary
Commerce,
Tidal
U.S.
23,
(1935).
L.Ed. 9
7. 296 U.S.
56 S.Ct.
Laguna Madre,
Characteristics
and Datums
(1995).
Texas
Id. at
tion’s NOAA’s reasoning by pointing disputed gap-filled in the from its the Madre Dr. expert, out that the Foundation’s area is nontidal is irrelevant because under Flick, measurements Luttes it is high evaluated water daily highest the water simply throughout Lagu- the at various locations averaged, regardless that is to be level were not cause, na. But Dr. Flick’s evaluations daily highest not the tide. the Id. at foot, because plus one line, Datum Plane at the Claunch/Lothrop the basis of requires. law the civil is not what And surveyed. already had been which require estab- And Luttes certainly doesn’t Claunch/Lothrop line was not based on can’t be at a line that lishing It tide. is mean of the True, jury says, the Court found. rely that the Foundation did telling Claunch/Lothrop line is found that anyone prove else to Dr. Flick or line of higher high tide the mean or above line, rely- of the mean tide actual location I know (although don’t Laguna Madre Claunch/Lothrop line. ing only on the line). how, this is no evidence of as there proof, failure in Undaunted the Foundation? help But how does Claunch/Lothrop concludes that the Court its is that proved Foundation All the Laguna’s margin west line must mark the by not measured boundary line was disputed because along property required by higher high tide mean of the at or conceded that that line is State has Luttes. There is no basis the civil law and Even daily high water levels. above mean decision or in fact for the Court’s law concession, that fact if the made that State boundary at property’s locate the missing proof does not establish —that Claunch/Lothrop line. boundary line suggested Foundation’s I suggests that erroneously The Court Every- high tide line. is the mean “position” Foundation’s accept would Foundation, one, it is including the knows that tide conclusion NOAA’s not. cannot Madre disputed area sure, maintains To be the Foundation suggestion That results be measured.13 that, reality and as- despite geophysical own being confused its from the Court suming Luttes doesn’t require tide to be “position” Foundation’s reasoning. The measure, boundary’s the line of any high level can be measured here, can be calculated higher high water mean, which water level produce at or Claunch/Lothrop and the line is Foundation, all that according to the *26 Flick that he calculated that Dr. testified law re- I don’t. The civil buys. Court disputed for the mean water by the to be measured quires the shoreline not But Flick admitted that he did area. tide, any just not water higher high in methodology performing use NOAA’s Luttes doesn’t hold otherwise. level. calculation, in he a his and that fact used said, Further, answering the as I’ve used methodology he himself had never Texas shorelines of whether question Essentially, Dr. Flick used non- before. higher high by the mean are measured measurements, factored them over tidal fact, tide, question of not answer the does he 18.6-year cycle, tidal and declared tide in this higher high whether the may He have found had found the mean. just It not measured. is case can be number, clearly not the mean a but it fails, its “position” Foundation’s by the contemplated level any of failure, the Court That proof as well. Court Luttes. in Claunch/Lothrop I The ignores. don’t. Luttes, line, boundary line the is the According to the civil law which and which Court proffered Foundation proper- of Texas seashore the boundaries no mean of reflects higher high today imposes, ties are at the mean of the much for Luttes at all. So a line water level tide. Luttes does permit using S.W.3d at 284. 13. 90 Furthermore, this bound- grant, then how do we resolve
controlling this case. there a the Foundation offered no evi- is reason principles. to first ary dispute? We return higher high of mean tide line. It dence locating for a appropriate The method Quite simply, can’t be found. as NOAA’s boundary legal question a for the is' concludes, can report no one measure boundary, locating court.14 And in Laguna. in of the this area overriding goal grantor’s is to follow the I refuses suspect reason Court Further, cases decided intent.15 civil-law problem present- the scientific confront before Luttes considered historical evi- in this case is because the Court con- ed substantially contemporaneous dence with Luttes cludes that has to apply. determining specific bound- grants property along margin dealt with the west Indeed, in Cava- ground. ary line on the lower and the Court Trevino, zos v. recognized the the Court notion that because has fixated on the importance of such evidence: of the characteristics of the sur- some par- which practical interpretation in this case are similar rounding property conduct have their ties interested surrounding to the characteristics instrument, property involved result to a written cases given land, this case must be identical. Court large body grant an ancient just wrong. granted by general de- asked for among always admitted as scription, Luttes and this
The difference between very best tests the intention of case is that we now know based work that the water movement NOAA’s the instrument. Thus, this area of the is non-tidal. the circum- construing grant, such a for the known formula we also know that attendant, at the time was stances tide, determining the mean of made, evidence for the competent are requires factoring the measure-
which in the same purpose placing the court 18.6-year cycle, over the tidal can- ments situation, it the same giving advan- result, As a we cannot applied. not be papers, which tages construing this water level’s mean. determine by the actors them- possessed were Therefore, insistence despite Court’s selves.16 contrary, Luttes and the civil-law control the simply rule it identifies cannot appro- evidence is Accordingly, historical end, In the the Court result this ease.. margin of the priate to determine the west me, proper- with for it locates the agrees grant civil-law be- Laguna Madre plus Datum Plane one ty’s boundary at the *27 determining rule for cause the civil-law line, it claims foot not the mean water level cannot be used. seashores calculated. can be Shine, Here, Darrell expert, the State’s II. THE WEST MARGIN the historical evidence correctly LOCATING examined MADRE
OF THE LAGUNA of the west mar- the location to determine original Madre that gin of line If no mean there is. Further, jury grantors intended. boundary of a civil-law to determine the 133, (1872) State, 6, (citing v. Tex. 163 14 16. 35 v. 12 S.W.3d Cavazos See Brainard 773, 784-85, (Tex. 1999). Trevino, (6 Wall.) 73 U.S. (1867)). L.Ed. 813 Co,, 151 Oil & Gas 15. Wheeler v. Stanolind 418, 149, (1952). Tex. 252 S.W.2d to establish the the area survey a line marks the mar- that the Shine found a That patent. boundary for issuance And there accuracy. reasonable gin with Spohn.17 v. in State was affirmed finding. judgment supporting is evidence Maddox judgment, F.M. the Spohn After experts it undisputed, Not was grant, and Big Barreta surveyed on the for sides testified based both field on the Maddox patent was issued surveys maps photo- and original survey generally Maddox’s *28 ade- boundary a but to ensure grant was is establish proved defendants And, claims sued, land. the Court quate grazing the east judgment and its identified vege- or rejected use of a bluff that Lwttes boundary grant ern of the as the boundary. ordered tation line as margin. Madre’s west The court d). 1135, (Tex.Civ.App.-1904, writ ref 17. 83 S.W. 1135 298 have to locate the arguments justifies boundary
But none of these would been history, they do ignoring mark, the Court nor typical- which is ordinary high water authority reject jury’s to find- provide vegetation a line of ly indicated ing reasonably the Shine line accu- unique physical erosion.21 Because of the rately margin of the La- locates the west Lake, characteristics of the no such line arguments guna Madre. The Court’s found, past pres- or the could blindly accepts if one make sense Moreover, variety of factors com- ent.22 Luttes controls irrespective of whether the fluctuations in the Lake’s produce bined to civil tide can be law’s level, to and causing water flood measured. large surrounding areas of recede from case, typical In the meander lines are flats.23 boundary not themselves a line.18 But the appointed by the Special The Master surveys are his- meander lines of earlier that “the mean- Supreme Court concluded surveyors torical of where the evidence most reason- der line is believed to be the mar- understood the Madre’s west boundary question.24 to be. And line is consistent able gin Shine’s answer” every surveyor with the evidence where Special Master also concluded Lothrop placed before Claunch and significant fixing historical data was margin. west adopted boundary.25 Supreme Court and issued his Special report Master’s Moreover, authority than the no less decree.26 recommended permit- Supreme United States Court has to establish a water ted meander lines grants, civil-law this Court Regarding boundary physical a case which the rejected original civil- absolutely has never question of the area in characteristics grant surveys as some evidence law other methods. impossible made it use as the grantor’s Interestingly, intent. dispute involving a series decisions discusses, observed that Court courts have about between the United States Utah original surveys not unusual for Lake, of the Great Salt and to be done for the contain excess land upon Court was called determine assessing payment due from purpose Lake when original boundary of the Utah ignored by But the Court grantee.27 A was admitted to the Union 1896.19 case, that the evidence indicates surveyed around meander line had been disputed that here the area opposite, segments beginning Lake in 1855 part grants. to not be was intended finally concluding 1966.20 The cus- Moreover, surveys maps subsequent locating method for the Lake’s tomary Gilbert, 429, See, 23. Id. at 253. e.g., v. 112 Tex. 18. Stover 841, (1923). 247 S.W. 842 24. Id. at 295. States, 461, v. 427 U.S. 96 19. See Utah United 3187, (1976). 49 625 S.Ct. L.Ed.2d 25. Id. at 301-02. Report Special in Utah v. United
20.
Master
245, 265,
States,
461,
reprinted
Utah,
in 1976 Utah
S.Ct.
Court using be located margin dre’s west cannot physical line have obvious 'character- would high That’s higher the mean of the tide. ground.29 on the istics only available water measure- because the Finally, suggests accept- Court Moreover, Foun- ments are non-tidal. line ing boundary the Shine as the its carry dation not failed to burden along confusion the entire case will create no jury, produced but it prove recognize I I disagree. Texas coastline. ’ line Claunch/Lothrop evidence that that the Luttes declaration about the civil margin west marks the Madre’s designed provide law was the benefits about Luttes. theory own even under its certainty stability for civil-law shore- line But the civil as a boundaries. mean of the Because the law, requires higher matter of the mean determined, and because tide cannot be case, high tide line to be used. In this changed since the margin the west has not fine cannot found as a of fact. be matter I would hold that the west original grants, Furthermore, I argument find Court’s evi- margin may located historical predictability about of shorelines ironic. substantially contemporaneous with dence today Not until this Court’s decision does Further, produced the State grants. argument the Foundation even have an line—the line—is evidence that its Shine at some property’s its the historical evidence sub- consistent with location different than where the historical with stantially contemporaneous today, evidence it to be. And with- shows grants physical and with evidence blush, out so much as a the Court chooses ai*ea. high disputed water mark boundary, proof Foundation’s I would there is some Consequently, hold that it deter- which shows was found jury’s finding supporting evidence the mean mining neither ac- line “marks with reasonable Shine other water. nor curacy line the fast land and between AND III. CLAIM PRECLU- ISSUE Thus, I Madre.” the shore FEES SION/ATTORNEYS’ the court of judgment affirm the would not, I Because the does appeals. Court dispose I would of the case Because grounds, on other I would must dissent. the State’s favor at 192 Id. 159 Tex. S.W.2d rehearing). (opinion on
APPENDIX 1 SOUTH TEXAS GULF COAST REGION *31 BELL, Appellant,
Walter
v. Texas. STATE
No. 74243. notes above that line. The Foundation position That’s the requires.
Notes
notes time of the graphs of the area from the survey. Both sur to the Cocke conformed physical the area’s grants present, grant Big Barreta veys confirm materially have not characteristics disputed property. did not include grants changed since the time of —two original grants well, in evidence were the historical evi- Also years. hundred As The surveys of the Little Barreta. intended grantors dence shows that surveyed by originally line to mark the Little Barreta vegetation the bluff or In la Fuente making Domingo de margin of the west survey of the made a confirmation boundary grants it of the Cocke the eastern two The meander lines grant. Little Barreta Big at issue—the Baretta and the Little closely de survey conform line based of the Cocke Baretta. And the Shine sketch. diagrammatic historical evidence. la Fuente’s largely on this ground also evidence on original grants, prior Physical Shine reviewed the Cole, an George line. surveys, early patent portions supports of the the Shine boundaries, tes- surveying water disputed property, photographs, expert historical that, cases, explained He prior court and information from tified for the State. tidal data are surveys He on aerial find a water when prior NOAA. overlaid available, surveyor would find the area and not photographs disputed of the ob- mark. ordinary high of the water changed served that the shoreline had not location physi- mark is a noticeably ordinary high the date since of the earliest ground by on the surveys, despite impressed cal feature construction water, changes vegeta- due to Waterway standing Intracoastal in the 1940s. in the soil itself. Cole testified tion or Furthermore, sur J.J. Cocke basically follows what Cole line Shine’s veyed Big sections of the Barreta to ordinary high would consider to be the railroad compa enable the State locate disputed water mark in the area. ny survey certificates area. did line, the Court part rejecting In Shine disputed include the area as sections, weight history by dismissive- proposed railroad but instead avoids the simply that Shine followed ly asserting part treated as a of the bed lines, previous surveyors’ meander Laguna Madre. the State sued lines in and of them- noting that meander predecessors-in- some of the Foundation’s also, interest, boundary. True selves are not the claiming unpatented the area as maintains, surveys original Although original grant land. Court State done to lost, grants land were not the court held that of civil-law had been
