"Don't feel bad, Sam. That peat bog did jump right in front of us out of nowhere."
A bog, quagmire or mire is a wetland that accumulates acidic peat, a deposit of dead plant material—often mosses or, in Arctic climates, lichens.
Bogs occur where the water at the ground surface is acidic, either from acidic ground water, or where water is derived entirely from precipitation, when they are termed ombrotrophic (rain-fed). Water flowing out of bogs has a characteristic brown colour, which comes from dissolved peat tannins. Bogs are very sensitive habitats and are of high importance for biodiversity.
Types of bog
Bog habitats may develop in various situations, depending on the climate and topography. The main types are:
Valley bog
These develop in gently sloping valleys or hollows. A layer of peat fills the deepest part of the valley, and a stream may run through the surface of the bog. Valley bogs may develop in relatively dry and warm climates, but because they rely on ground or surface water, they only occur on acidic substrates.
Raised bog
These develop from a lake or flat marshy area, over either non-acidic or acidic substrates. Over centuries there is a progression from open lake, to marsh, then fen (or on acidic substrates, valley bog) and carr, as silt or peat fill the lake. Eventually peat builds up to a level where the land surface is too flat for ground or surface water to reach the centre of the wetland. This part therefore becomes wholly rain-fed (ombrotrophic), and the resulting acidic conditions allow the development of bog (even if the substrate is non-acidic). The bog continues to form peat, and over time a shallow dome of bog peat develops: a raised bog. The dome is typically a few metres high in the centre, and is often surrounded by strips of fen or other wetland vegetation at the edges or along streamsides, where ground water can percolate into the wetland.
Blanket bog
In cool climates with consistently high rainfall, the ground surface may remain waterlogged for much of the time, providing conditions for the development of bog vegetation. In these circumstances bog develops as a layer "blanketing" much of the land, including hilltops and slopes. Although blanket bog is more common on acidic substrates, under some conditions it may also develop on neutral or even alkaline ones, if abundant acidic rainwater predominates over the ground water. Blanket bog cannot occur in drier or warmer climates, because under those conditions hilltops and sloping ground dry out too often for peat to form – in intermediate climates blanket bog may be limited to areas which are shaded from direct sunshine. In periglacial climates a patterned form of blanket bog may occur, known as string bog.
Quaking bog
Quaking bog or schwingmoor is a form of bog occurring in wetter parts of valley bogs and raised bogs, and sometimes around the edges of acidic lakes where bog is beginning to form. The bog vegetation forms a mat half a metre or so thick, floating over water or very wet peat. Walking on this surface causes it to move – larger movements may cause visible ripples of the surface, or they may even make trees sway.
Named after the daughter of King George II, [Princess Anne] boasted a population of 2,200 souls.
Anne, Princess Royal and Princess of Orange (2 November 1709 – 12 January 1759) was the second child and eldest daughter of King George II of Great Britain and his consort, Caroline of Ansbach. She was the spouse of William IV, Prince of Orange, the first hereditary stadtholder of the Netherlands. Princess Anne was the second daughter of a British sovereign to hold the title Princess Royal. She was Regent of the Netherlands from 1751 until her death in 1759, exercising extensive powers on behalf of her son William V. Because of her English upbringing and family connections, she was known as an Anglophile - despite being unable to convince the Dutch Republic to enter the Seven Years' War on the side of the British.
With a population just under 2400 people, this hamlet at the head of the Manokin River was named for Princess Anne of Great Britain, daughter of King George II. It was established in 1733 and serves as the county seat for Somerset County (the southernmost county in Maryland).
In the mid-18th century, Princess Anne gained considerable importance as a market center because of the river trade. This was later augmented by the southward extension of the Eastern Shore Railroad on Maryland's Eastern Shore. At that time, the Manokin River was navigable as far as the bridge at Princess Anne.
Much of the town's architectural heritage from those days has been preserved. About 150 acres (0.61 km2) of the old town, containing about 300 structures, is entered on the National Register of Historic Places as the Princess Anne Historic District.
As he reached the turn-in, a black Buick Lucerne sedan pulled out.
The Buick Lucerne is a full-size car sold by the Buick division of General Motors. Introduced at the 2005 Chicago Auto Show, the Lucerne replaced both the Park Avenue and the LeSabre for the 2006 model year, and was sold through the 2011 model year. The Lucerne was based on a revised H-body platform, which it shared with the late Pontiac Bonneville.
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