1.
Camp Pathfinder
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Camp Pathfinder is a boys Summer camp in Algonquin Provincial Park, Ontario, Canada. The camp is best known for its canoe tripping program, Pathfinder follows a tradition of using wood and canvas canoes. Several other camps in Algonquin and elsewhere follow a tradition of tripping with. Pathfinders canoes are painted a bright red. The current director is Michael Sladden, Camp Pathfinder was founded in 1914 by William Bennett and Franklin Gray. In 1922, the camp was sold to Herman J, chief Norton, who became one of Pathfinders most influential owners. Pathfinder was almost shut down or sold to the Ontario Provincial Government when the government told Norton the lease for the camp would not be renewed, the government later renewed the lease and the camp remained in operation. Since then, owners or co-owners have included Frank J. Horton, Bill Swift, Roy Thrall, Mac Rand, Glen Arthurs, Camp Pathfinder is located on Source Lake, in Algonquin Provincial Park, just more than a mile away from Highway 60. Source Lake is a point to the Algonquin Park canoe route system. There are no campsites on Source Lake, there are, however, a few residential cabins and the camp itself on the lake. The camp is located on an island in the lake, commonly referred to as Camp Pathfinder Island or CPI, on the opening days of each session, the whole camp meets at the new Indian council ring, and a meeting introducing the camp session is held. This meeting, and other aspects of the camp, have a number of traditions, for example, there is a site believed be the grave of a First Nations man known as Algonquin Joe, and it is traditional to put a fallen leaf on the site. The camp also features a course and climbing walls. Recently, the camp completed its 100th season, Pathfinder has an extensive canoe tripping program. Trip duration and destination varies by age group of the campers on the trip, the youngest campers normally stay within the boundaries of Algonquin Park or very close to. The older campers venture on longer and more challenging trips with varying destinations, paddles Flashing in the Sun, The Stories of Pathfinder in Algonquin Park
2.
Algonquin Provincial Park
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Algonquin Provincial Park is a provincial park located between Georgian Bay and the Ottawa River in Southern Ontario, Canada, mostly within the Unorganized South Part of Nipissing District. Established in 1893, it is the oldest provincial park in Canada, additions since its creation have increased the park to its current size of about 7,653 square kilometres. For comparison purposes, this is one and a half times the size of Prince Edward Island or about a quarter of the size of Belgium. The park is contiguous with several smaller, administratively separate provincial parks that protect important rivers in the area, resulting in a larger total protected area. Its size, combined with its proximity to the urban centres of Toronto and Ottawa, makes Algonquin one of the most popular provincial parks in the province. Highway 60 runs through the south of the park, while the Trans-Canada Highway bypasses it to the north, over 2,400 lakes and 1,200 kilometres of streams and rivers are located within the park. Some notable examples include Canoe Lake and the Petawawa, Nipissing, Amable du Fond, Madawaska and these were formed by the retreat of the glaciers during the last ice age. The park is considered part of the border between Northern Ontario and Southern Ontario, the park is in an area of transition between northern coniferous forest and southern deciduous forest. This unique mixture of forest types, and the variety of environments in the park, allows the park to support an uncommon diversity of plant. It is also an important site for wildlife research, Algonquin Park is the only designated park within the province of Ontario to allow industrial logging to take place within its borders. In the 19th century, the industry harvested the large white pine and red pine trees to produce lumber for domestic and American markets. The loggers were followed by numbers of homesteaders and farmers. Even at that time, however, the beauty was recognized by nature preservationists. To manage these conflicting interests, the Ontario Government appointed a commission to inquire into and report on the matter. The act to establish Algonquin Park was drawn up in 1892 by this five member Royal Commission, made up of Alexander Kirkwood, James Dickson, Archibald Blue, Robert Phipps, and Aubrey White. The commissioners remarked in their report, the experience of older countries had shown that the wholesale. Only licenses to cut pine would be issued, the commissioners had recommended that when the hardwood was mature, it too should be cut. Researchers believe that smoke from a forest fire in Algonquin Park was responsible for New Englands Dark Day of May 19,1780 and this is based on investigations into scar marks which are left in the growth rings of trees that survive forest fires
3.
New France
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The territory was divided into five colonies, each with its own administration, Canada, Hudsons Bay, Acadia, Newfoundland, and Louisiana. Acadia had a history, with the Great Upheaval, remembered on July 28 each year since 2003. The descendants are dispersed in the Maritime Provinces of Canada, in Maine and Louisiana in the United States, with populations in Chéticamp, Nova Scotia. In the sixteenth century, the lands were used primarily to draw from the wealth of natural resources, in the seventeenth century, successful settlements began in Acadia, and in Quebec by the efforts of Champlain. By 1765, the population of the new Province of Quebec reached approximately 70,000 settlers. In 1763 France had ceded the rest of New France, except the islands of Saint Pierre and Miquelon, to Great Britain and Spain at the Treaty of Paris, in 1800, Spain returned its portion of Louisiana to France under the secret Treaty of San Ildefonso. However, French leader Napoleon Bonaparte in turn sold it to the United States in the Louisiana Purchase of 1803, New France eventually became part of the United States and Canada, with the only vestige remaining under French rule being the tiny islands Saint Pierre and Miquelon. In the United States, the legacy of New France includes numerous placenames as well as pockets of French-speaking communities. In Canada, institutional bilingualism and strong Francophone identities are arguably the most enduring legacy of New France, the Conquest is viewed differently among Francophone Canadians, and between Anglophone and Francophone Canadians. Around 1523, the Florentine navigator Giovanni da Verrazzano convinced King Francis I, late that year, Verrazzano set sail in Dieppe, crossing the Atlantic on a small caravel with 50 men. After exploring the coast of the present-day Carolinas early the year, he headed north along the coast. The first European to discover the site of present-day New York, he named it Nouvelle-Angoulême in honour of the king, verrazzanos voyage convinced the king to seek to establish a colony in the newly discovered land. Verrazzano gave the names Francesca and Nova Gallia to that land between New Spain and English Newfoundland, in 1534, Jacques Cartier planted a cross in the Gaspé Peninsula and claimed the land in the name of King Francis I. It was the first province of New France, however, initial French attempts at settling the region met with failure. French fishing fleets continued to sail to the Atlantic coast and into the St. Lawrence River, French merchants soon realized the St. Lawrence region was full of valuable fur-bearing animals, especially the beaver, which were becoming rare in Europe. Eventually, the French crown decided to colonize the territory to secure, another early French attempt at settlement in North America took place in 1564 at Fort Caroline, now Jacksonville, Florida. Intended as a haven for Huguenots, Caroline was founded under the leadership of René Goulaine de Laudonnière and it was sacked by the Spanish led by Pedro Menéndez de Avilés who then established the settlement of St. Augustine on 20 September 1565. Acadia and Canada were inhabited by indigenous nomadic Algonquian peoples and sedentary Iroquoian peoples and these lands were full of unexploited and valuable natural riches, which attracted all of Europe
4.
Louisiana (New France)
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Louisiana or French Louisiana was an administrative district of New France. Under French control 1682 to 1762 and 1802 to 1803, the area was named in honor of King Louis XIV, by French explorer René-Robert Cavelier, Louisiana was divided into two regions, known as Upper Louisiana, which began north of the Arkansas River, and Lower Louisiana. The U. S. state of Louisiana is named for the historical region, although French exploration of the area began during the reign of Louis XIV, French Louisiana was not greatly developed, due to a lack of human and financial resources. France regained sovereignty of the territory in the secret Treaty of San Ildefonso of 1800. But strained by obligations in Europe, Napoleon Bonaparte decided to sell the territory to the United States in the Louisiana Purchase of 1803, the United States ceded part of the Louisiana Purchase to the United Kingdom in the Treaty of 1818. This section lies above the 49th parallel north in a portion of present-day Alberta, in the 18th century, Louisiana included most of the Mississippi River Valley, from what is now the Midwestern United States south to the coast of the Gulf of Mexico. Both areas were dominated numerically by Native American tribal populations, at times, fewer than two hundred soldiers were assigned to all of the colony, on both sides of the Mississippi. In the mid-1720s, Louisiana Indians numbered well over 35,000, to the east was territory disputed with the British colonies on the Atlantic seaboard, the French claim extended to the Appalachian Mountains. The Rocky Mountains marked the extent of the French claim. The general flatness of the land aided movement through the territory, the topography becomes more mountainous towards the west, with the notable exception of the Ozark Mountains, which are located in the mid-south. A colonial government soon emerged, with its capital originally at Mobile, later at Biloxi, the government was led by a Governor-general, and Louisiana became an increasingly important colony in the early 18th century. French exploration of the area began with the 1673 expedition of Louis Joliet and Jacques Marquette, as noted above, Upper Louisiana was primarily settled by colonists from French Canada. There was further substantial intermarriage and integration with the local Illinois peoples, French settlers were attracted by the availability of arable farmland as well as by the forests, abundant with animals suitable for hunting and trapping. Genevieve across the river in todays Missouri, the region was initially governed as part of Canada, but was declared to be part of Louisiana in 1712, with the grant of the Louisiana country to Antoine Crozat. Thus, Vincennes and Peoria were the limit of Louisianas reach, the outposts at Ouiatenon, Chicago, Fort Miamis, and Prairie du Chien operated as dependencies of Canada. Those fleeing British control founded outposts such as the important settlement of St. Louis and this became a French fur-trading center, connected to trading posts on the Missouri and Upper Mississippi rivers, leading to later French settlement in that area. In the 1762 Treaty of Fontainebleau, France ceded Louisiana west of the Mississippi River to Spain, its ally in the war, even after France had lost its claim to Louisiana, settlement of Upper Louisiana by French-speakers continued for the next four decades. French explorers and frontiersmen, such as Pedro Vial, were employed as guides and interpreters by the Spanish
5.
Rapids
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Rapids are sections of a river where the river bed has a relatively steep gradient, causing an increase in water velocity and turbulence. Rapids are hydrological features between a run and a cascade, rapids are characterised by the river becoming shallower with some rocks exposed above the flow surface. As flowing water splashes over and around the rocks, air bubbles become mixed in with it and portions of the surface acquire a white colour, forming what is called whitewater. Rapids occur where the bed material is resistant to the erosive power of the stream in comparison with the bed downstream of the rapids. Very young streams flowing across solid rock may be rapids for much of their length, rapids cause water aeration of the stream or river resulting in better water quality. Rapids are categorized in classes, generally running from I to VI, a Class 5 rapid may be categorized as Class 5. 1-5.9. While class I rapids are easy to negotiate and require no maneuvering, river rafting sports is carried out where many rapids are there in the course
6.
Fan waterfalls
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A waterfall is a place where water flows over a vertical drop or a series of drops in the course of a stream or river. Waterfalls also occur where meltwater drops over the edge of an iceberg or ice shelf. Waterfalls are commonly formed in the course of a river. At these times the channel is narrow and deep. When the river courses over resistant bedrock, erosion happens slowly, as the watercourse increases its velocity at the edge of the waterfall, it plucks material from the riverbed. Whirlpools created in the turbulence as well as sand and stones carried by the increase the erosion capacity. This causes the waterfall to carve deeper into the bed and to recede upstream, often over time, the waterfall will recede back to form a canyon or gorge downstream as it recedes upstream, and it will carve deeper into the ridge above it. The rate of retreat for a waterfall can be as high as one, eventually, the outcropping, more resistant cap rock will collapse under pressure to add blocks of rock to the base of the waterfall. Waterfalls normally form in an area due to erosion. After a long period of being formed, the water falling off the ledge will retreat. Eventually, as the pit grows deeper, the waterfall collapses to be replaced by a steeply sloping stretch of river bed, a river sometimes flows over a large step in the rocks that may have been formed by a fault line. Waterfalls can occur along the edge of a trough, where a stream or river flowing into a glacier continues to flow into a valley after the glacier has receded or melted. The large waterfalls in Yosemite Valley are examples of this phenomenon, another reason hanging valleys may form is where two rivers join and one is flowing faster than the other. Waterfalls can be grouped into ten classes based on the average volume of water present on the fall using a logarithmic scale. Class 10 waterfalls include Niagara Falls, Paulo Afonso Falls and Khone Falls, young Wrote Waterfalls, form and process this work made waterfalls a much more serious topic for research for modern Geoscientists. Ledge waterfall, Water descends vertically over a cliff, maintaining partial contact with the bedrock. Block/Sheet. Classical, Ledge waterfalls where fall height is equal to stream width. Curtain, Ledge waterfalls which descend over a larger than the width of falling water stream
7.
Indigenous peoples of the Americas
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The indigenous peoples of the Americas are the pre-Columbian peoples of the Americas and their descendants. The term Amerindian is used in Quebec, the Guianas, Indigenous peoples of the United States are commonly known as Native Americans or American Indians, and Alaska Natives. Application of the term Indian originated with Christopher Columbus, who, in his search for Asia, eventually, the Americas came to be known as the West Indies, a name still used to refer to the islands of the Caribbean Sea. This led to the blanket term Indies and Indians for the indigenous inhabitants, although some indigenous peoples of the Americas were traditionally hunter-gatherers—and many, especially in the Amazon basin, still are—many groups practiced aquaculture and agriculture. The impact of their agricultural endowment to the world is a testament to their time, although some societies depended heavily on agriculture, others practiced a mix of farming, hunting, and gathering. In some regions the indigenous peoples created monumental architecture, large-scale organized cities, chiefdoms, states, and empires. Many parts of the Americas are still populated by peoples, some countries have sizable populations, especially Belize, Bolivia, Chile, Ecuador, Greenland, Guatemala, Mexico. At least a different indigenous languages are spoken in the Americas. Some, such as the Quechuan languages, Aymara, Guaraní, Mayan languages, many also maintain aspects of indigenous cultural practices to varying degrees, including religion, social organization, and subsistence practices. Like most cultures, over time, cultures specific to many indigenous peoples have evolved to incorporate traditional aspects, some indigenous peoples still live in relative isolation from Western culture and a few are still counted as uncontacted peoples. The specifics of Paleo-Indian migration to and throughout the Americas, including the dates and routes traveled, are the subject of ongoing research. According to archaeological and genetic evidence, North and South America were the last continents in the world with human habitation. During the Wisconsin glaciation, 50–17,000 years ago, falling sea levels allowed people to move across the bridge of Beringia that joined Siberia to northwest North America. Alaska was a glacial refugium because it had low snowfall, allowing a small population to exist, the Laurentide Ice Sheet covered most of North America, blocking nomadic inhabitants and confining them to Alaska for thousands of years. Indigenous genetic studies suggest that the first inhabitants of the Americas share a single population, one that developed in isolation. The isolation of these peoples in Beringia might have lasted 10–20,000 years, around 16,500 years ago, the glaciers began melting, allowing people to move south and east into Canada and beyond. These people are believed to have followed herds of now-extinct Pleistocene megafauna along ice-free corridors that stretched between the Laurentide and Cordilleran Ice Sheets. Another route proposed involves migration - either on foot or using primitive boats - along the Pacific Northwest coast to the south, archeological evidence of the latter would have been covered by the sea level rise of more than 120 meters since the last ice age
8.
Canoe
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A canoe is a lightweight narrow boat, typically pointed at both ends and open on top, propelled by one or more seated or kneeling paddlers facing the direction of travel using a single-bladed paddle. In International Canoe Federation nomenclature used in some European countries such as the United Kingdom the term refers to kayaks. Canoes are used for racing, whitewater canoeing, touring and camping, freestyle, the intended use of the canoe dictates its hull shape and length and construction material. Historically, canoes were dugouts or made of bark on a wood frame, most modern canoes are made of molded plastic or composites such as fiberglass. Until the mid-1800s the canoe was an important means of transport for exploration and trade, canoeing has been part of the Olympics since 1936. In places where the played a key role in history, such as the northern United States, Canada, and New Zealand. Canoes can be adapted to many purposes, for example with the addition of sails, outboard motors, the word canoe comes from the Carib kenu, via the Spanish canoa. Constructed between 8200 and 7600 BC, and found in the Netherlands, the Pesse canoe may be the oldest known canoe, excavations in Denmark reveal the use of dugouts and paddles during the Ertebølle period. Australian Aboriginal people made canoes using a variety of materials, including bark, the indigenous people of the Amazon commonly used Hymenaea trees. Many indigenous peoples of the Americas built bark canoes and they were usually skinned with birch bark over a light wooden frame, but other types could be used if birch was scarce. At a typical length of 4.3 m and weight of 23 kg, although susceptible to damage from rocks, they are easily repaired. When you reach them you load canoe and baggage upon your shoulders and go overland until the navigation is good, and then you put your canoe back into the water, and embark again. American painter, author and traveler George Catlin wrote that the canoe was the most beautiful. Native American groups of the north Pacific coast made dugout canoes in a number of styles for different purposes, from western red-cedar or yellow-cedar, different styles were required for ocean-going vessels versus river boats, and for whale-hunting versus seal-hunting versus salmon-fishing. The Quinault of Washington State built shovel-nose canoes, with double bows, the Kootenai of British Columbia province made sturgeon-nosed canoes from pine bark, designed to be stable in windy conditions on Kootenay Lake. The first explorer to cross the North American continent, Alexander Mackenzie, used extensively, as did David Thompson. Its dimensions were, length approximately 11 m, beam 1.2 to 1.8 m and it could carry 60 packs weighing 41 kg, and 910 kg of provisions. With a crew of eight or ten, they could make three knots over calm waters, four to six men could portage it, bottom up
9.
Canal
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Canals and navigations are human-made channels for water conveyance, or to service water transport vehicles. In the vernacular, both are referred to as canals, and in most cases, the works will have a series of dams. These areas are referred to as water levels, often just called levels. In contrast, a canal cuts across a drainage divide atop a ridge, many canals have been built at elevations towering over valleys and others water ways crossing far below. Cities need a lot of water and many canals with sources of water at a higher level can deliver water to a destination where there is a lack of water. The Roman Empires Aqueducts were such water supply canals, a navigation is a series of channels that run roughly parallel to the valley and stream bed of an unimproved river. A navigation always shares the drainage basin of the river, a vessel uses the calm parts of the river itself as well as improvements, traversing the same changes in height. A true canal is a channel that cuts across a drainage divide, most commercially important canals of the first half of the 19th century were a little of each, using rivers in long stretches, and divide crossing canals in others. This is true for many canals still in use, there are two broad types of canal, Waterways, canals and navigations used for carrying vessels transporting goods and people. These can be subdivided into two kinds, Those connecting existing lakes, rivers, other canals or seas and oceans and those connected in a city network, such as the Canal Grande and others of Venice Italy, the gracht of Amsterdam, and the waterways of Bangkok. Aqueducts, water canals that are used for the conveyance and delivery of potable water for human consumption, municipal uses, hydro power canals. Historically canals were of importance to commerce and the development, growth. In 1855 the Lehigh Canal carried over 1.2 million tons of burning anthracite coal, by the 1930s the company which built. By the early 1880s, canals which had little ability to compete with rail transport, were off the map. In the next couple of decades, coal was diminished as the heating fuel of choice by oil. Later, after World War I when motor-trucks came into their own, Canals are built in one of three ways, or a combination of the three, depending on available water and available path, Human made streams A canal can be created where no stream presently exists. Either the body of the canal is dug or the sides of the canal are created by making dykes or levees by piling dirt, stone, the water for the canal must be provided from an external source, like streams or reservoirs. Where the new waterway must change elevation engineering works like locks, lifts or elevators are constructed to raise, examples include canals that connect valleys over a higher body of land, like Canal du Midi, Canal de Briare and the Panama Canal
