Helliwell v. State

183 So. 2d 286, 1966 Fla. App. LEXIS 5535
CourtDistrict Court of Appeal of Florida
DecidedFebruary 15, 1966
DocketNo. 65-458
StatusPublished
Cited by1 cases

This text of 183 So. 2d 286 (Helliwell v. State) is published on Counsel Stack Legal Research, covering District Court of Appeal of Florida primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Helliwell v. State, 183 So. 2d 286, 1966 Fla. App. LEXIS 5535 (Fla. Ct. App. 1966).

Opinion

SWANN, Judge.

The appellant, Paul L. E. Helliwell, was the plaintiff below. The appellees, The State of Florida and The Trustees of the Internal Improvement Fund of Florida, were the defendants.

The plaintiff filed a suit to quiet title to an area containing approximately 62.36 acres of partially submerged land in Biscayne Bay, consisting of “salt marsh and mangrove fiáis”, lying west and north of Mashta Island, in Dade County, Florida. This land will be referred to herein as “Mashta flats”. The plaintiff claimed that fee simple title to these flats was (1) included in mesne conveyances from the defendants to his predecessors in title, and (2) that title became vested in his predecessors under and by virtue of the Riparian Act of 1856.

The defendants’ answer denied these allegations and alleged that “Mashta flats” was sovereign land, covered by the waters [287]*287of Biscayne Bay at high tide; that the defendants had not sold or conveyed the land in question to anyone; and counterclaimed for a decree adjudicating the land to be sovereign in character and owned by the State of Florida in fee simple.

Both parties consented to the appointment of a Special Master. The Honorable Richard H. Hunt was appointed, conducted numerous hearings and filed his reports, which were confirmed and adopted by the chancellor. The plaintiff appeals the final decree declaring the fee simple title to the land in question to be vested in the State of Florida.

The reports of the Special Master contained, in part, the following:

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“Mr. Matheson testified that the offshore flats or submerged lands claimed by plaintiff are covered over with water at high tide, although at low tide one or more spots of sand bar emerge from the water. His testimony generally corresponded with that given by other witnesses in establishing that the submerged area sought by plaintiff is covered by water and generally navigable by small craft at high tide.
“At the second hearing, plaintiff called as a witness one John M. Arribas, a civil engineer who recently conducted test borings on and near the lands in suit to determine the types and characteristics of soil and other material which underlie the water bottoms in question, as well as the type and character of soil to be found under the nearby upland and improved land area; and to give opinion evidence as to the differences found to exist, viz., the type of soil and land structure under the bay bottom and that under the surface of the adjoining land area.
“This witness testified that the borings established that the same soil and rock structures existed in each spot tested (see markings made on plaintiff’s exhibit 32), except that organic matter, being the remnants of decomposed mangrove trees, roots and weeds, were removed from the three bore holes which were sunk on the upland spots, whereas no such organic material came up from the marginal water borings.
“This tends to support other testimony in the case that the submerged lands sought by plaintiff have always been unobstructed tidal waters of the main body of Biscayne Bay and have never been marsh or swamp in character, or within the mangrove uplands area which long since has been filled and bulkheaded at the point in question.
“This witness also testified that the aqueous area in suit was completely covered by water at high tide when the bore tests were in progress.”
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“1. Plaintiff’s title derives from (a) deed dated October 19, 1895, from Trustees of the Internal Improvement Fund of the State of Florida to Waters S. Davis, shown as Entry No. 29 in the abstract of title in evidence, conveying lands on Key Biscayne described as Sections 4, 5, 6, 8 and 9, ‘including Salt Marsh and Mangrove Flats’. Later on, upon application of attorneys representing plaintiff’s predecessor in title, the Trustees of the Internal Improvement Fund granted a second or amended deed to The Biscayne Company on behalf of the Matheson interests, dated May 9, 1922, which conveyed to the said title owner ‘All of Section 6 * * * according to plat of J. E. Hilgard’. (Emphasis supplied)
“The aforesaid deeds are in the record as plaintiff’s exhibits 1 and 2, respectively.
“The.plat of J. E. Hilgard was established as of 1870 (defendants’ exhibit 1) and shows as ‘S. W. Point’, the area involved in this suit. Attached to said [288]*288plat, as defendants’ exhibit 3, is a communication from the U. S. General Land Office, Department of the Interior, to the Commissioner of Agriculture at Tallahassee, which reflects that 24 acres of land existed in Section 6, of which the point of land known as ‘S. W. Point’ which forms the subject matter of this suit under the name of Mashta Island, comprised a portion of said 24-acre estimate.
“Prior to the 1870 survey by Hilgard, a certified state survey made in 1847 (in the record as defendants’ exhibit 2) shows areas of 'saw palmetto land’ and describes almost the entire western half of Biscayne Key as ''salt marsh and mangrove flats’.
“It is significant that the general outline and contour of the S. W. Point area is clearly depicted in this survey and does not appear to include the bay bottom area now claimed by plaintiff in this action.
“Defendants’ exhibit 6 is a chart of the Florida Reefs published by the federal government in 1856 and shows 'S. W. Point’ almost exactly as said area appears in the I-Iilgard map of 1870.
“Defendants’ exhibits 7 and 8 are U. S. Coast and Geodetic Survey charts of 1861 and 1878, respectively, and show 'coral banks covered with sand’ in the marginal off-shore sections of Key Biscayne. These charts essentially show the same ‘S. W. Point’ area and outlying bay bottoms which line the entire western side of Biscayne Key in varying depths and distances. Without clear evidence to the contrary, the master is convinced without any doubt that the shoal area claimed by plaintiff falls in the same classification as other off-shore shallow water areas touching the western side of Biscayne Key, which waters are navigable and at high tide completely cover the occasional shallow bars lying in the bay offshore from the uplands.
“Defendants’ exhibits 9, 10 and 11 are charts published by the federal government in 1892,1907 and 1919, respectively, and each carries out the similarity of contours and location of said ‘S. W. Point’ as has above been noted to exist from the very first chart of record.
“Defendants’ exhibit 13 is a U. S. Coast and Geodetic topographic map made from air photographs and which shows ‘S. W. Point’ after filling and improvement by plaintiff’s predecessor in title. As of this time, a virtual ‘hook’ had been dredged and constructed into the bay at the end of the point for the formation of a boat basin and erection of a two-story residence structure. The ‘shoal area’ continues to be shown as such, as do other similar areas lying along the same shoreline.
“Defendants’ exhibit 22 is a U. S.

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Related

Helliwell v. State
192 So. 2d 487 (Supreme Court of Florida, 1966)

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Bluebook (online)
183 So. 2d 286, 1966 Fla. App. LEXIS 5535, Counsel Stack Legal Research, https://law.counselstack.com/opinion/helliwell-v-state-fladistctapp-1966.