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Big Talbot Island State Park
Big Talbot Island State Park is a state park in Florida, United States. It is located on Big Talbot Island, a coastal barrier island 20 miles east of downtown Jacksonville on A1A North and immediately north of Little Talbot Island State Park along the Atlantic coastal plain. The park is a nature preserve and a location for nature study, bird-watching, or photography. Other activities include hiking, bicycling, fishing, boating, canoeing, kayaking, and picnicking. Amenities include picnic pavilions, nature trails, a fishing pier, a boat ramp, bike trails and beaches. The park is open from 8:00 am till sundown year round. The coastal landscape and beach at Big Talbot Island is unique within the state of Florida for its rock-like sedimentary hardpan soil deposits underlying the surface. Where these formations are exposed in the shallow waters surrounded the island they provide habitat for molluscs, crabs, oysters, and other tide pool creatures. The formations and sand on Blackroc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Duval County, Florida
Duval County is in the northeastern part of the U.S. state of Florida. As of the 2020 census, the population was 995,567, up from 864,263 in 2010. Its county seat is Jacksonville, Florida, with which the Duval County government has been consolidated since 1968. Duval County was established in 1822, and is named for William Pope Duval, Governor of Florida Territory from 1822 to 1834. Duval County is the central county of the Jacksonville Metropolitan Statistical Area. History This area had been settled by varying cultures of indigenous peoples for thousands of years before European contact. Within the Timucuan Ecological and Historic Preserve in Jacksonville, archeologists have excavated remains of some of the oldest pottery in the United States, dating to 2500 BCE. Prior to European contact, the area was inhabited by the Mocama, a Timucuan-speaking group who lived throughout the coastal areas of northern Florida. At the time Europeans arrived, much of what is now Duval Count ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trailhead
A trailhead is the point at which a trail begins, where the trail is often intended for hiking, biking, horseback riding, or off-road vehicles. Modern trailheads often contain rest rooms, maps, sign posts and distribution centers for informational brochures about the trail and its features, and parking areas for vehicles and trailers. The United States Access Board states "A trailhead is defined as an outdoor space that is designated by an entity responsible for administering or maintaining a trail to serve as an access point to the trail." The intersection of two trails is a trail junction and does not constitute a trailhead. Historically, the cities located at the terminus of major pathways for foot traffic such as the Natchez Trace and the Chisholm Trail were also known as trailheads. For mountain climbing and hiking, the elevation of the trailhead above sea level is posted to give an idea of how high the mountain is above the Height above average terrain, average terrain. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quercus Virginiana
''Quercus virginiana'', also known as the southern live oak, is an evergreen oak tree endemic to the Southeastern United States. Though many other species are loosely called live oak, the southern live oak is particularly iconic of the Old South. Many very large and old specimens of live oak can be found today in the Deep South region of the United States. Description Although live oaks retain their leaves nearly year-round, they are not true evergreens. Live oaks drop their leaves immediately before new leaves emerge in the spring. Occasionally, Senescence, senescing leaves may turn yellow or contain brown spots in the winter, leading to the mistaken belief that the tree has oak wilt, whose symptoms typically occur in the summer. A live oak's defoliation may occur sooner in marginal climates or in dry or cold winters. The Bark (botany), bark is dark, thick, and furrowed longitudinally. The leaves are stiff and leathery, with the tops shiny dark green and the bottoms pale gra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Machaba Balu Preserve
The Machaba Balu Preserve is a nature preserve encompassing of protected lands in northeastern Florida, just to the northeast of Jacksonville, at the confluence of the Nassau, the St. Marys, and the St. Johns Rivers as they flow toward the Atlantic Ocean through a wide network of islands, canals, and tidal marshes. The name ''Machaba Balu'' means "saved marsh" in the language of the Timucua people, who occupied the area in pre-Columbian times and met the first European explorers of the region; the Timucua never used this name themselves, however, as it is a modern language construct. The preserve, created with land purchased in 2002 mostly from Alcoma Corporation by the Nature Conservancy, includes 77 islands and numerous individual tracts of tidal marshland between the Nassau and the St. Johns Rivers. The largest clusters lie to the west of Little Talbot Island State Park and on either side of Sisters Creek south of the large fork. The Nature Conservancy chose to preserve the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tidal Marsh
A tidal marsh (also known as a type of "tidal wetland") is a marsh found along rivers, coasts and estuaries which floods and drains by the tidal movement of the adjacent estuary, sea or ocean. Tidal marshes are commonly zoned into lower marshes (also called intertidal marshes) and upper or high marshes, based on their elevation above sea level. A middle marsh zone also exists for tidal freshwater marshes. Tidal marshes may be further classified into back-barrier marshes, estuarine brackish marshes and tidal freshwater marshes, depending on the influence of sea level. Coastal Coastal tidal marshes are found within coastal watersheds and encompass a variety of types including fresh and salt marshes, bottomland hardwood swamps, mangrove swamps, and palustrine wetlands. Island and barrier island Tidal Marshes also form between a main shoreline and barrier islands. These elongated shifting landforms evolve parallel and in close proximity to the shoreline of a tidal marsh. Many becom ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Estuary
An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environments and are an example of an ecotone. Estuaries are subject both to marine influences such as tides, waves, and the influx of saline water, and to fluvial influences such as flows of freshwater and sediment. The mixing of seawater and freshwater provides high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world. Most existing estuaries formed during the Holocene epoch with the flooding of river-eroded or glacially scoured valleys when the sea level began to rise about 10,000–12,000 years ago. Estuaries are typically classified according to their geomorphological features or to water-circulation patterns. They can have many different names, such as bays, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hammock (ecology)
Hammock is a term used in the southeastern United States for stands of trees, usually hardwood, that form an ecological island in a contrasting ecosystem. Hammocks grow on elevated areas, often just a few inches high, surrounded by wetlands that are too wet to support them. The term ''hammock'' is also applied to stands of hardwood trees growing on slopes between wetlands and drier uplands supporting a mixed or coniferous forest. Types of hammocks found in the United States include tropical hardwood hammocks, temperate hardwood hammocks, and maritime or coastal hammocks. Hammocks are also often classified as hydric (wet soil), mesic (moist soil) or xeric (dry soil). The types are not exclusive, but often grade into each other. Unlike many ecosystems of the coastal plain of the southeastern United States, hammocks are not tolerant of fire. Hammocks tend to occur in locations where fire is not common, or where there is some protection from fire in neighboring ecosystems. Hammocks ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Florida Scrub
Florida sand pine scrub is an endangered subtropical forest ecoregion found throughout Florida in the United States. It is found on coastal and inland sand ridges and is characterized by an evergreen xeromorphic plant community dominated by shrubs and dwarf oaks. Because the low-nutrient sandy soils do not retain moisture, the ecosystem is effectively an arid one. Wildfires infrequently occur in the Florida scrub. Most of the annual rainfall (about ) falls in summer. It is endangered by residential, commercial and agricultural development, with the largest remaining block in and around the Ocala National Forest. Lake Wales Ridge National Wildlife Refuge also holds a high proportion of remaining scrub habitat, while the Archbold Biological Station near Lake Placid contains about of scrub habitat and sponsors biological research on it. Plant communities There is a high level of endemism in the flora and fauna, including an estimated 40 species of plants, 4 vertebrates and at least ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beach
A beach is a landform alongside a body of water which consists of loose particles. The particles composing a beach are typically made from rock, such as sand, gravel, shingle, pebbles, etc., or biological sources, such as mollusc shells or coralline algae. Sediments settle in different densities and structures, depending on the local wave action and weather, creating different textures, colors and gradients or layers of material. Though some beaches form on inland freshwater locations such as lakes and rivers, most beaches are in coastal areas where wave or current action deposits and reworks sediments. Erosion and changing of beach geologies happens through natural processes, like wave action and extreme weather events. Where wind conditions are correct, beaches can be backed by coastal dunes which offer protection and regeneration for the beach. However, these natural forces have become more extreme due to climate change, permanently altering beaches at very rapid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Timucuan Ecological And Historic Preserve
The Timucuan Ecological and Historic Preserve is a U.S. National Preserve in Jacksonville, Florida. It comprises of wetlands, waterways, and other habitats in northeastern Duval County. Managed by the National Park Service in cooperation with the City of Jacksonville and Florida State Parks, it includes natural and historic areas such as the Fort Caroline National Memorial and the Kingsley Plantation. The preserve was established in 1988 and expanded in 1999 by Preservation Project Jacksonville. Background The Fort Caroline National Memorial is located in the Timucuan Preserve, as is the Kingsley Plantation, the oldest standing plantation in the state. The Preserve is maintained through cooperation by the National Park Service, the Florida Department of Environmental Protection and the City of Jacksonville Department of Parks and Recreation. It is named for the Timucua Indians who had 35 chiefdoms throughout northern Florida and south Georgia at the time of Spanish colonizati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lord Chancellor
The lord chancellor, formally the lord high chancellor of Great Britain, is the highest-ranking traditional minister among the Great Officers of State in Scotland and England in the United Kingdom, nominally outranking the prime minister. The lord chancellor is appointed by the sovereign on the advice of the prime minister. Prior to their Union into the Kingdom of Great Britain, there were separate lord chancellors for the Kingdom of England (including Wales) and the Kingdom of Scotland; there were lord chancellors of Ireland until 1922. The lord chancellor is a member of the Cabinet and is, by law, responsible for the efficient functioning and independence of the courts. In 2005, there were a number of changes to the legal system and to the office of the lord chancellor. Formerly, the lord chancellor was also the presiding officer of the House of Lords, the head of the judiciary of England and Wales and the presiding judge of the Chancery Division of the High Court of Justic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charles Talbot, 1st Baron Talbot
Charles Talbot, 1st Baron Talbot, (168514 February 1737) was a British lawyer and politician. He was Lord High Chancellor of Great Britain from 1733 to 1737. Life Talbot was the eldest son of William Talbot, Bishop of Durham, a descendant of the 1st Earl of Shrewsbury. He was educated at Eton and Oriel College, Oxford, and became a fellow of All Souls College in 1704. He was called to the bar in 1711, and in 1717 was appointed solicitor general to the prince of Wales. Having been elected a member of the House of Commons in 1720, he became Solicitor General in 1726, and in 1733 he was made Lord Chancellor and raised to the peerage with the title of Lord Talbot, Baron of Hensol, in the County of Glamorgan. Talbot proved himself a capable equity judge during the three years of his occupancy of the Woolsack. Among his contemporaries he enjoyed the reputation of a wit; he was a patron of the poet James Thomson, who in '' The Seasons'' commemorated a son of his to whom he acte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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