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[2] [3] The registered owner of a property in question is normally presumed, sometimes conclusively, to be the legal owner of the property and is said to “hold the title” or is “registered on the title”. Ownership of property usually implies a right of possession, as opposed to the party that has right of property.
Conservation easements may result in a significant reduction in the sale price of the land because a builder can no longer develop it. In fact, this difference in value is the basis for the granting of the original tax incentives. An estimate of 35%–65% value reduction has been made on conservation easement land to the land owner. [13]
In the United States, a plat (/ p l æ t / [1] or / p l ɑː t /) [2] (plan) is a cadastral map, drawn to scale, showing the divisions of a piece of land. United States General Land Office surveyors drafted township plats of Public Lands Surveys to show the distance and bearing between section corners, sometimes including topographic or ...
The Land Registry has been dealing with the registration of all transactions (purchase, sale, mortgage, remortgage and other burdens) concerning registered land since 1892, and issued land certificates which are a state guarantee of the registered owner's good title up to 1 January 2007. Land Certificates have been abolished by virtue of ...
A land parcel or cadastral parcel is defined as "a continuous area, or more appropriately volume, that is identified by a unique set of homogeneous property rights". [3] Cadastral surveys document the boundaries of land ownership, by the production of documents, diagrams, sketches, plans (plats in the US), charts, and maps. They were originally ...
Topographic maps are also commonly called contour maps or topo maps. In the United States, where the primary national series is organized by a strict 7.5-minute grid, they are often called or quads or quadrangles. Topographic maps conventionally show topography, or land contours, by means of contour lines.
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Also amphidrome and tidal node. A geographical location where there is little or no tide, i.e. where the tidal amplitude is zero or nearly zero because the height of sea level does not change appreciably over time (meaning there is no high tide or low tide), and around which a tidal crest circulates once per tidal period (approximately every 12 hours). Tidal amplitude increases, though not ...