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Last modified
2/27/2024 11:59:28 AM
Creation date
2/13/2024 10:47:48 AM
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Official Documents
Official Document Type
Application
Approved Date
02/15/2000
Control Number
2000-044
Agenda Item Number
7.J.
Subject
National Register Application for Multi-Property District
Jungle Trail Enhancement Project
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F1 <br />i <br />• <br />14PS Farm 10-900-0 <br />United States Department of the Interior <br />National Park Service <br />National Register ofHistoric Places <br />Continuation Sheet <br />Section number —L Page 3 - <br />OMBRppmalW 1024-0719 <br />South Hole Midden <br />events. The marginal areas contained shell, but less black organic midden stain. Dickel (1992) also notes that <br />boundary determination along the estuary edge to the northwest can be problematic, where the midden shell grades <br />into natural shell deposits. Richards (1990) reported the depth of midden deposits to the east of US AIA ranging <br />from 75 cm. to 1 meter, which may reflect the non-marginal midden deposits to the west as well. <br />APPEARANCE OF THE SITE DURING THE PREHISTORIC OCCUPATION <br />Judging the appearance of the South bole Midden site during prehistoric occupation is a daunting task. The <br />shoreline of Orchid Island is subject to dynamic geomorphic changes. On the one hand. in addition to the normal <br />erosive action of wind, wave, and current, and the catastrophic action of many storm events, the sea level along the <br />Atlantic coast has been rising at a rate of approximately I cm. per 25 years for the last 3000 years, or about 1 meter <br />if we accept a basal date of 500 B.C. In addition, at various times inlets to the north of South Hole have naturally <br />formed and sealed in several locations, alternatively allowing and denying the outfall of Indian River water, fed <br />by terrestrial runoff, into the Atlantic Ocean. On the other hand, current water management canals and impermeable <br />urban ground surfaces effectively shuttle terrestrial water into the Indian River, the onslaught being somewhat offset <br />by the inlets, or outfalls, that have been fixed in place during the twentieth century. <br />When the inlet has been closed in the past it has linked the area of Orchid 'Island to the long narrow peninsula <br />extending down from Cape Canaveral and would have allowed the easy migration of terrestrial animal species to <br />populate the island. Terrestrial animal species inhabiting the island at various times include a variety of birds, <br />reptiles, w mphibians, and mammals that could have been exploited for food by prehistoric and historic human <br />pupu:auuats, Addii unally, about 2555 spxiub oli'fish and u number of crustaceans, mollusks, marine mammals, and <br />marine turtles exist off the Atlantic shore of the island and about 400 species of fish, 200 mollusks, and many other <br />animals exist in the Indian River lagoon (Jones 1990:10-11). <br />The site, nonetheless, very likely was a prominence, though relatively diminutive, as it lay protected in the lee of <br />the primary dune. it is also likely that the natural inlet at one time flowed nearby to the north in the vicinity of <br />News Cut. Similar middens adjacent to natural inlets also occur at Gilbert's Bar in Martin County and at .Jupiter <br />Inlet in Rilm Peach County, half: lo-crted to the south along the Indian Rivct. Wiwi: coastal hastttnock would have <br />been predominant on the higher elevations of the site. As elevation decreased, vegetation would trend into the <br />various species of spranna, junc'us, distichlis, and other salt tolerant ,grasses of the high marsh and, finally, into the <br />mangrove fringc of the Indian River estuary (Myers and Cwef 1990). <br />
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