The trestle was pushed more than a metre out of alignment. In 1922, an earlier steel truss bridge, located slightly upstream of the trestle, was destroyed when impounded logs broke free following heavy rains and crashed into the bridge. 4) remains.Ī a concrete road bridge ( New Brunswick Highway 105) crosses the stream at Hartland paralleled by a Canadian Pacific Railway trestle (now part of The Great Trail). Only the Ellis Bridge (North Becaguimec No. 1), which was constructed in 1948, burned in 2009. 3), which was constructed in 1909, burned in 2011. The Mangrum or Stormdale Bridge (Becaguimec Stream No. Three covered bridges once crossed the Becaguimec Stream, though only one remains standing. Settlement of the Becaguimec Valley itself began with the establishment of the community of Rockland in 1825 and Coldstream in or about 1826. Mouth of 'Guimac was renamed Hartland in 1860. Several more families soon followed and a community coalesced known as Mouth of 'Guimac. The first European settler to arrive at the mouth of the Becaguimec was Loyalist William Orser in 1797. One of the earliest records of permanent settlement at this site indicates that in 1790 a Wolastoqiyik man by the name of Governor Toma was found "tilling his cornfield" at the mouth of the Becaguimec. The hill above the south bank of the stream's mouth (Hagerman's Hill) made an exceptional look-out point from which several miles up the Saint John River can be seen. ![]() The fertile land at the mouth of the Becaguimec has likely been inhabited for millennia. The name "Becaguimec" literally means "the place where the salmon lie." The construction of the hydroelectric dam at Mactaquac Dam in 1967 has since decimated the salmon population in the Saint John River. The Wolastoqiyik (Maliseet) people named the river for the bountiful salmon pool which lay at the mouth of the stream. The best time of year for fishing trout is from mid-May to mid-June, after the sediment clears from the water after the thaw, but before the summer heat increases the water temperature. The notable fish species found predominantly in the upper reaches of the Becaguimec are brown trout and rainbow trout. The Becaguimec enters the Saint John River at the town of Hartland, the site of the world's longest covered bridge. There are several notable eddies and Class 2 rapids along this stretch, not the least of which is known as Hell's Eddy, 2 miles upstream from the stream's mouth. The gradient of the stream increases from Mill Brook towards the Saint John River. The stream is slow-paced and meandering between the forks and Mill Brook near Ashland, not infrequently changing course because of floods. After that point the stream is sometimes called the Mainstream, from which the adjacent community derives its name. Where the North and South Branches meet is known as the Becaguimec Forks, lying just northwest of the intersection of Provincial Highway 104 and Provincial Highway 575. The South Branch flows from Becaguimec Lake 13 kilometres southeast of the community of Cloverdale. The North Branch originates in three tiny lakes only a short distance west of the upper reaches of the Nashwaak River: Malcolm Lake, Long Lake and Owl Lake respectively. ![]() The Cold Stream originates from springs on the western slope of Skedaddle Ridge and the eastern slope of Garvie Mountain in the community of Knowlesville. Three primary branches, the North Branch Becaguimec, the South Branch Becaguimec and the Cold Stream compose the Becaguimec Stream.
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