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You are here: BAILII >> Databases >> England and Wales Court of Appeal (Civil Division) Decisions >> Loose v Lynn Shellfish Ltd & Ors [2014] EWCA Civ 846 (19 June 2014) URL: http://www.bailii.org/ew/cases/EWCA/Civ/2014/846.html Cite as: [2014] EWCA Civ 846, [2015] Ch 547, [2014] WLR(D) 280, [2015] 2 WLR 643 |
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ON APPEAL FROM THE HIGH COURT OF JUSTICE
CHANCERY DIVISION
Sir William Blackburne
Strand, London, WC2A 2LL |
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B e f o r e :
LORD JUSTICE PITCHFORD
and
LORD JUSTICE KITCHIN
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JOHN HENRY LOOSE |
Claimant/ Respondent |
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- and - |
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LYNN SHELLFISH LIMITED and Others |
Defendants/Appellants |
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and MICHAEL GEORGE LE STRANGE MEAKIN |
Part 20 Defendant/Respondent |
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Mr. Tim Calland and Miss Jennifer Meech (Instructed by Charles Russell LLP) for the Part 20 Defendant/appellant
Mr. Michael Davey Q.C. (instructed by Parkinson Wright LLP) for the respondent
Hearing dates : 7th & 8th May 2014
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Crown Copyright ©
Lord Justice Moore-Bick :
Background
The topography
"12. The nature of the claims of the estate, and therefore of Mr Loose whose leased fishing rights are said to be co-extensive with those of the estate, is very much bound up with the shifting nature of the sandbanks and channels which are so much a feature of the eastern side of the Wash. I was taken in this regard to a series of charts going back over four centuries. The earliest was from 1588, the year of the Spanish Armada, and the next (and rather more informative) Henry Bell Chart (so-named after the person during whose mayoralty of King's Lynn the chart was drawn) was from 1693. In those days King's Lynn exercised an admiralty jurisdiction in its area of the Wash. Those and later charts show that whereas in earlier times tidal waters ran close to the shoreline of the area bordered by the relevant lordships, with clearly marked sandbanks separated from the foreshore at low tide, nevertheless with the passage of time and the effect of siltation and other natural phenomena the fresh water and tidal channels altered, both in terms of width and of direction, so that what were once distinct sandbanks became, when exposed at low water, part of the foreshore and thus accessible on foot from the shoreline. A striking example of this process is provided by the so-called Stubborn Sand. In the 16th and 17th centuries, this appears on the charts as an island at low tide, separated from the shore on its eastern side by a distinct channel of water and on its western side by what was known as the Old Channel. It was not then accessible on foot from dry land. The Old Channel led to King's Lynn which lies to the immediate south and served as a navigable means of access to that port. By the 19th century Stubborn Sand had become and has since remained, when exposed at low water, a part of the foreshore. In effect it has ceased to be distinguishable as a distinct sand bank although it continues to bear that name. Indeed, as the later charts show, the Old Channel has long ceased to be a navigable channel and is nowadays really no more than a tongue of water when exposed at low tide: access by boat to King's Lynn must now be by a channel lying further to the west
13. Another example of the process of change in this part of the Wash concerns the line of what is known as Wolferton Creek. This is a fresh water outlet draining the land between Wolferton and Sandringham on the Norfolk coast to the east. In the earlier charts and maps this stream is shown as flowing into the Wash at low water in roughly an east/west direction. Later charts show the flow of the stream at low water as following a more northerly course. Its gradual shift to the north gave rise to a dispute as to the precise position of the fishery's southern boundary. The details do not matter. In Le Strange v Lynn Corporation , to which I have already referred, the issue was settled by a determination that the boundary was the east/west line followed by the stream in earlier days
14. Other sandbanks, notably the Sunk and Ferrier Sands, have ceased to be distinct "islands" at low tide. Both are now accessible on foot from the shoreline where it is bordered by the estate lordships. Although once it did not, the estate, and through it Mr Loose, now claims that its fishery extends seaward over sands which are now identified on contemporary charts (moving from north to south) as the South Sunk Sand, the Outer Ferrier Sand, the Ferrier Sand and (as to its northern part) the Peter Black Sand. These were formerly inaccessible at low water from dry land but with the silting up of the channels that once separated them from the dry land are now accessible on foot at low water from the eastern shoreline. . . . "
For convenience there is annexed to this judgment a copy of the chart of the area that was attached to his judgment.
Public and private rights
"the common people of England have regularly a liberty of fishing in the sea or arms thereof, as a public common of piscary, and may not without injury to their right be restrained of it, unless in such places, creeks, or navigable rivers where either the King or some particular subject hath gained a propriety exclusive of that common liberty."
"The soil of "navigable tidal rivers," like the Shannon, so far as the tide flows and reflows, is prima facie in the Crown, and the right of fishery prima facie in the public. But for Magna Charta, the Crown could, by its prerogative, exclude the public from such prima facie right, and grant the exclusive right of fishery to a private individual, either together with or distinct from the soil. And the great charter left untouched all fisheries which were made several, to the exclusion of the public, by Act of the Crown not later than the reign of Henry II.
If evidence be given of long enjoyment of a fishery, to the exclusion of others, of such a character as to establish that it has been dealt with as of right as a distinct and separate property, and there is nothing to show that its origin was modern, the result is not that you say, this is usurpation, for it is not traced back to the time of Henry II, but that you presume that the fishery being reasonably shown to have been dealt with as property, must have become such in due course of law, and therefore must have been created before legal memory."
Loose v Castleton
"That, then, being the law, one must next turn to see what were the facts in so far as they bore on the question of the seaward boundary of the le Strange several fishery. First, there were the series of leases of fishery rights that had been granted at various dates ranging from 1857 up to 1970. If one looks at the earliest and latest of the leases in that series, one finds this. There is a lease from 1857 to 1867 that defines the seaward boundary of the fishery rights that were demised as "the extreme low-water mark of the sea on the extreme west." The two latest leases are one from 1965 to 1970, in which the demise was of "the foreshore and so much of the sea-bed as belongs to the landlord," and, finally, the current lease under which the plaintiff in this action claims, which defines the seaward boundary in these words: "… as far as can be worked without boats at extreme low water which lie within the landlord's fishery." Those are the first pieces of evidence supporting the view, for which the plaintiff contended and which the judge accepted, that the seaward boundary extended at least to the mean low-water mark of spring, as opposed to ordinary, tides. Secondly, there was evidence, in particular from a Mr. Thursby, who was very familiar with the rights as they had in fact been exercised, that de facto the le Strange estate and its lessees had claimed and worked the mussel scalps between the low-water mark of ordinary tides and the low-water mark of spring tides for at least 17 years prior to this litigation. Finally, however, and perhaps most importantly of all, there was clear evidence, which the judge accepted, that the best mussel grounds, the favourite habitat of the mussel on this length of coast, lay between the low-water mark of ordinary tides and the low-water mark of spring tides. In the light of that evidence, one is entitled to ask oneself the question: is it really to be supposed that, when the Crown was granting to favoured subjects a valuable right such as a several fishery relating to shellfish in the tenth or the eleventh century, it was doing so by reference to an artificial line on a map — mean low water at ordinary tides — that, so far as I am aware, is a purely modern concept that emerged in the nineteenth century, and doing so in order to deny to the favoured subjects the primary benefit that one would suppose was intended to be conferred on them, namely the benefit of exploiting the fishery where it could best be exploited? The answer to this question is, obviously: "no, one would not suppose that." "
"If, however, the court adopts the approach — as, of course, it must — set out in a few simple words by Willes J. in Malcolmson v. O'Dea, which Bridge L.J. has already read, the whole approach to the case becomes comparatively simple. It is plain from the paragraph in Willes J.'s advice to the House of Lords that, once there has been established over a long period of time — and, of course, what is a long period of time will vary from case to case — a succession of acts of purported ownership in relation to a fishery such as this, the court will, as Willes J. said, assume, or presume, that the claimant to such rights was at all times acting lawfully and not unlawfully. . .
Following the principles of Malcolmson v. O'Dea, I would answer the question by saying that there is clear evidence of claim to ownership extending over 100 years in the whole of this area; there is nothing to indicate a modern origin for that right, and nothing in the historical documents to negative, or render uncertain or unsound, the presumption of a lost grant. I therefore agree that the plaintiff succeeds on the first issue in this case.
I can deal very briefly with the other two issues. So far as the extent of the fishery is concerned, I venture to think that it is totally artificial to suppose, or to argue, that there is any particular limit on the seaward side of the fishery. We have to approach this matter on the basis that, at least in theory, we are dealing with a right that was at some time the subject of a grant from the Crown—and it has to be, owing to Magna Carta, a grant prior in date to 1189. I doubt very much whether, in 1189, those who were granting rights of fishery were particularly concerned about tide levels of any particular description. What they were granting was the right to fish for shellfish—and shellfish from "the shore," or "the foreshore." Prima facie, it would seem to me, once a several fishery is established, unless there is some evidence to the contrary one would suppose that that fishery extends far enough to enable the grantee to get the fish (mussels in this case) where they normally grow. We have seen the evidence of Dr. Loose as to the habits of mussels. It is not, therefore, to my mind, necessary or useful, or anything but artificial, to try to limit a fishery such as this by reference to some purely abstract line on a chart. I say "abstract" because all "means" are of necessity abstract, and it would be quite ludicrous to try to apply a line on a chart to the physical conditions prevailing in an estuary such as this. As Mr. Claiborne said more than once, obviously the seaward boundary of this fishery will shift; there will be changes in the tide and changes, perhaps, in sandbanks in the neighbourhood there, or even possibly elsewhere. The ordinary, sensible conclusion must be that the fishery extends to where the mussels are exposed at low tide, wherever that is. So I again agree with the judge on that."
The issues in this case
The nature and scope of the estate's rights
"The Order with which we are concerned is the Lynn Deeps Order 1872. Paragraph 2 of this Order begins with the words: "The following are the description and limits of the fishery (as shown on plans deposited at the Board of Trade and marked 'Lynn Deeps Fishery Order 1872')"—and then the Order proceeds to define the limits of the fishery. The language of the Order describing the landward boundary of the deep-sea fishery in the relevant area does indeed refer to the low-water mark of ordinary tides. The interpretation of the Order was the subject of litigation between the corporation of King's Lynn and the then holder of the title to the le Strange estate in 1885. One of the results of that litigation was that it was held that, in view of the words at the opening of paragraph 2 of the Order, "(as shown on plans deposited [etc.])," where there was a conflict between the deposited plans and the express language of the Order the plans were to prevail. The plans annexed to the Order, and, indeed, to its successor, the Lynn Deeps Order 1932 , show, as the boundary between the statutory area conferred on the corporation of King's Lynn and the le Strange estate on this length of coastline, not mean low-water mark but the Admiralty chart datum line, which is at least as far seaward as, if not further seaward than, the mean low-water mark of spring tides.
Finally, on this subject, it is to be observed that in the current Order, that of 1932, there is an express reservation of the right of the le Strange estate in the words to be found in article 19 : "Nothing in this Order contained shall take away lessen prejudice or interfere with any right power or privilege of Charles Alfred le Strange Esquire his executors administrators or assigns … ."
Accretion
" . . . their Lordships find it advisable to consider briefly the nature of the doctrine of accretion. This is a doctrine which gives recognition to the fact that where land is bounded by water, the forces of nature are likely to cause changes in the boundary between the land and the water. Where these changes are gradual and imperceptible (a phrase considered further below), the law considers the title to the land as applicable to the land as it may be so changed from time to time. This may be said to be based on grounds of convenience and fairness. Except in cases where a substantial and recognisable change in boundary has suddenly taken place (to which the doctrine of accretion does not apply), it is manifestly convenient to continue to regard the boundary between land and water as being where it is from day to day or year to year. To do so is also fair. If part of an owner's land is taken from him by erosion, or diluvion (i.e. advance of the water) it would be most inconvenient to regard the boundary as extending into the water: the landowner is treated as losing a portion of his land. So, if an addition is made to the land from what was previously water, it is only fair that the landowner's title should extend to it. The doctrine of accretion, in other words, is one which arises from the nature of land ownership from, in fact, the long-term ownership of property inherently subject to gradual processes of change."
Accretion – the grounds of appeal
The seaward boundary of the fishery
Lord Justice Pitchford :
Lord Justice Kitchin :