James' World 2

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Banff National Park is Canada’s oldest national park, established in 1885. Located in Alberta’s Rocky Mountains, 110–180 kilometers (68–112 mi) west of Calgary, Banff encompasses 6,641 square kilometers (2,564 sq mi) of mountainous terrain, with many glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbors to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial center of the park is the town of Banff, in the Bow River valley.

The Canadian Pacific Railway was instrumental in Banff’s early years, building the Banff Springs Hotel and Chateau Lake Louise, and attracting tourists through extensive advertising. In the early 20th century, roads were built in Banff, at times by war internees from World War I, and through Great Depression-era public works projects. Since the 1960s, park accommodations have been open all year, with annual tourism visits to Banff increasing to over 5 million in the 1990s. Millions more pass through the park on the Trans-Canada Highway. As Banff has over three million visitors annually, the health of its ecosystem has been threatened. In the mid-1990s, Parks Canada responded by initiating a two-year study which resulted in management recommendations and new policies that aim to preserve ecological integrity.

Banff National Park has a subarctic climate with three ecoregions, including montane, subalpine, and alpine. The forests are dominated by Lodgepole pine at lower elevations and Engelmann spruce in higher ones below the treeline, above which is primarily rocks and ice. Mammal species such as the grizzly bear, cougar, wolverine, elk, bighorn sheep, and moose are found, along with hundreds of bird species. Reptiles and amphibians are also found but only a limited number of species have been recorded. The mountains are formed from sedimentary rocks which were pushed east over newer rock strata, between 80 and 55 million years ago. Over the past few million years, glaciers have at times covered most of the park, but today are found only on the mountain slopes though they include the Columbia Icefield, the largest uninterrupted glacial mass in the Rockies. Erosion from water and ice have carved the mountains into their current shapes. Wikipedia

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Kalamazoo is a city in the southwest region of the U.S. state of Michigan. It is the county seat of Kalamazoo County. As of the 2010 census, Kalamazoo had a population of 74,262. Kalamazoo is the major city of the Kalamazoo-Portage Metropolitan Statistical Area, which has a population of 335,340 as of 2015. Kalamazoo is equidistant from the major American cities of Chicago and Detroit, each less than 150 miles (240 kilometers) away.

One of Kalamazoo’s most notable features is the Kalamazoo Mall, an outdoor pedestrian shopping mall. The city created the mall in 1959 by closing part of Burdick Street to auto traffic, although two of the mall’s four blocks have been reopened to auto traffic since 1999. Kalamazoo is home to Western Michigan University, a large public university, Kalamazoo College, a private liberal arts college, and Kalamazoo Valley Community College, a two-year community college.

Originally known as Bronson (after founder Titus Bronson) in the township of Arcadia, the names of both the city and the township were changed to “Kalamazoo” in 1836 and 1837, respectively. The name “Kalamazoo” comes from a Potawatomi word, first found in a British report in 1772. The Kalamazoo River, which passes through the modern city of Kalamazoo, was located on the route between Detroit and Fort Saint-Joseph (nowadays Niles, Michigan). French-Canadian traders, missionaries, and military personnel were quite familiar with this area during the French era and thereafter. The Kalamazoo River was then known by Canadians and French as La rivière Kikanamaso. The name “Kikanamaso” was also recorded by Father Pierre Potier, a Jesuit missionary for the Huron-Wendats at the Assumption mission (south shore of Detroit), while en route to Fort Saint-Joseph during the fall of 1760. Legend has it that “Ki-ka-ma-sung”, meaning “boiling water”, referred to a footrace held each fall by local Native Americans, in which participants had to run to the river and back before a pot boiled. The word negikanamazo, purported to mean “otter tail” or “stones like otters”, has also been cited as a possible origin of the name. Another theory is that it means “the mirage or reflecting river”. Another legend is that the image of “boiling water” referred to fog on the river as seen from the hills above the current downtown. The name was also given to the river that flows almost all the way across the state.

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Cathedral Rock is a natural sandstone butte on the Sedona skyline and one of the most-photographed sights in Arizona, United States. The rock formation is located in the Coconino National Forest in Yavapai County, about a mile (1.6 km) west of Arizona Route 179, and about 2.5 miles (4.0 km) south of the “Y” intersection of Routes 179 and 89A in uptown Sedona. The summit elevation of Cathedral Rock is 4,967 feet (1,514 m).

The Cathedral Rock trail (USFS Trail #170) is a popular short, steep ascent from the Back O’ Beyond trailhead to the saddle points or “gaps” in Cathedral Rock.

Geologically, Cathedral Rock is carved from the Permian Schnebly Hill formation, a redbed sandstone formed from coastal sand dunes near the shoreline of the ancient Pedregosa Sea. Ripple marks are prominent along the lower Cathedral Rock trail, and a black basalt dike may be seen in the first saddle.

Cathedral Rock was called “Court House Rock” on some early maps, and Courthouse Butte was called “Church House Rock”, which has caused endless confusion ever since.

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An image from Cathedral Rock Sedona

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