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The Northumberland Strait varies in depth between 17 and 65 metres, with the deepest waters at either end. The tidal patterns are complex; the eastern end has the usual two tides per day, with a tidal range of 1.2 to 1.8 metres, while the western end effectively has only one tide per day.
"A league and a labor" (4,605.5 acres; 18.638 km 2) was a common first land grant [4] and consisted of a league of land away from the river plus one extra labor of good riparian (river-situated) land. A headright of this much land was granted to "all persons [heads of families] except Africans and their descendants and Indians living in Texas ...
Day, James M. (1964) Maps of Texas, 1527-1900: The Map Collections of the Texas State Archives, Austin: The Pemberton Press, pp. 13, 15–18, 20, 23, 25, 32 Taliaferro, Henry G.; Jane A. Kenamore and Uli Haller (1988) Cartographic Sources in the Rosenberg Library , Category:College Station, Texas : Texas A&M University Press for the Rosenberg ...
The second map shows a partition of the counties into 12 regions of Texas, as defined by the Texas comptroller. The table, further below, reports currently listings by county, updated frequently. [a] Regions are defined by the Texas State Comptroller, who has partitioned the state into 12 regions for economic performance reporting, as shown here.
The geography of Texas is diverse and large. Occupying about 7% of the total water and land area of the U.S., [1] it is the second largest state after Alaska, and is the southernmost part of the Great Plains, which end in the south against the folded Sierra Madre Oriental of Mexico.
Map of the Northumberland Strait. In Canadian ghostlore , the Ghost Ship of Northumberland Strait is a ghost ship said to sail ablaze within the Northumberland Strait , the body of water that separates Prince Edward Island from Nova Scotia and New Brunswick in eastern Canada .
Shaded relief map of the Llano Estacado. Texas contains a wide variety of geologic settings. The state's stratigraphy has been largely influenced by marine transgressive-regressive cycles during the Phanerozoic, with a lesser but still significant contribution from late Cenozoic tectonic activity, as well as the remnants of a Paleozoic mountain range.
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