The original Name Whimpys' is in the next town here, Ostervile. Near Oyster Harbors. RE BELOW: ""..but steam and sulfur are still emitted..""I guess they tried Oyster Burgers but it didn't catch on. A picture of cartoon Whimpy is on the sign. They serve breakfast also. September I was out ( an R in the Month ) to Kingman Arizona, at the Dam Bar and Steakhouse. At RT 66 and Andy Devine Avenue. Nice Old Classic Bar, had dinner there. Went into the Bar and waited for the food to cook. The place had an Oyster Bar. So far in from the Sea. I said to my self why would I eat Oysers in The Dam Bar. I decided that I didn'r need any. Within 2 days I was climbing in a little known Cavern called Grand Canyon some 500 feet under the ground, carved Limestones all over. It had a passageway years ago that let a surface vent allow for a fall in some what 7,000 yrs ago of a 9 FT Tall Ground Slouth which was discovered decades ago and Taxidermed so it is an Exhibit. I never saw a Ground Slouth before. I saw Limestone caves befor but this brings t mind one fact that we must remember. Limestones in contact to with intruded into Granites can produce a change in rock chemistry that can be a reason that metals collect and form; Contact Metamorphism. I suspect based upon some talks recently that we have that stuff in Mazama. Goodies are more Free Milling Style and more Oxide Chemistry rather than Sulphide Based Chemistry and hense more economic. I hope that is the case with The Snows of Killa Mazama. I like that part, the prior drillers forgot to assay for GOLD at 100% of the old cores! ChuckaWhat Time is it in Mazama? We await the report, The Bigga Deposit at Mazama. The Deposit is a Kili Mazama, much likle Kilimanjaro. I say TITLE the Report : Kilimazama. climbingkilimanjaro.com ""..Climbing Kilimanjaro, a comprehensive guide to climbing Mount Kilimanjaro by Destination Africa Tours. Mt Kilimanjaro: 005.00 degrees south, 036 degrees east, 5895m a.m.s.l. Crowned by an eternal snow cap, Mt. Kilimanjaro is situated inside the Kilimanjaro National Park in Tanzania, it is the highest mountain in Africa and the tallest free-standing mountain on earth. This guide aims to provide the potential Kilimanjaro climber with valuable and accurate information on climbing Kilimanjaro, which will hopefully contribute towards increasing your chances of a successful summit attempt. Detailed itineries, maps, useful links, stunning pictures and photography cover all the major routes, including the Marangu, Machame, Umbwe, Mweka, Shira, Lemosho, Rongai, Maua, Loitokitok, and Arrow Glacier routes. To further assist you with your preparation on hiking or trekking to the summit of this breathtaking mountain, we have included essential information and tips on your mental and physical preparation, a fitness program, and a list of all equipment required. Other useful information provided, included a printable final checklist, food, porters, guides, important health issues, how to get there and hotels and transfers.
ONE STOP BOOKING SERVICE Destination Africa Tours have 7 years of experience in leading clients to the summit. Our experienced guides have a proud success rate of 96%+ and have safely guided over 2700 clients to the peak. Our professional tour consultants have all made successful summit attempts and are therefore in a position to provide you with an in depth knowledge on a planned summit attempt. We provide unique and tailor-made itineraries to suite your individual requirements and preferences, including all your accommodation bookings, meet and assist at the airport, airport transfers, as well as many exciting excursion extensions to the surrounding game reserves and the magical island of Zanzibar.
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PS The Geology READ: volcano.und.nodak.edu Kilimanjaro, Tanzania Location: 3.07 S, 37.35 E Elevation: 19,335.6 ft (5,895m)
Kilimanjaro is a giant stratovolcano reaching an elevation of 19,335.6 ft. (5,895 m). Other names for this volcano are: Kilima Dscharo, Oldoinyo Oibor (white mountain in Masai), and Kilima Njaro meaning shining mountain in Swahili. This volcano's highest and youngest cone is named Kibo. Shira to the west and Mawenzi in the east are older cones that make up Kilimanjaro. Kibo has not been active in modern times, but steam and sulfur are still emitted. At the top of Kibo's summit is a 1 1/2 mile (2 1/4 Km) wide crater.
Kilimanjaro is the largest of an E-W belt of about 20 volcanoes near the southern end of the East African Rift Valley. Also prominent in this belt are Ngorongoro caldera - a superb wildlife refuge, Ol Donyo Lengi - a carbonitite volcano, and Meru. Kilimanjaro is a triple volcano with the youngest and central peak of Kibo being 7.5-8.7 miles (12-14 km) from Shira to the west and Mawenza to the east. As all of Kilimanjaro's climbers know the gentle lower slopes steepen to 30 degrees about 13,000 ft.(4 km) elevation.
Shira is topped by a broad plateau, perhaps a filled caldera, and erosion has cut deeply into a remnant rim. In contrast, Mawenzi's summit is a steep rocky peak surrounded by cliffs 1,600 ft.(0.5 km) to 4,900 ft.(1.5 km) high. Erosion has removed the original crater, and a great horseshoe shaped ridge opens to the northeast. Mile-deep gullies with 30-45 degree gradients make many places practically inaccessible. Massive series of radial and concentric dyke swarm make up more than 30-40 percent of the summit area of Mawenzi. Kibo's glacier-clad summit, the highest spot in Africa, is a 1.2 x 1.7 mile (1.9 x 2.7 km) caldera, with an inner crater nearly a mile (1.3 km) wide, and inside that a deep, 1,148 ft. (350 m) wide central pit. Original volcanic forms are preserved at the summit and on many of the flanks, except on the south side where glaciers have cut deeply into the cone. Nearly 250 satellitic cones occur on Kilimanjaro, most following SE and NW trends. Estimates suggest that of a total volume of about 1,150 cu. miles, Mawenzi and Shira each contribute roughly 120 cu. mi. of andesites and basalts, Kibo has the same volume of similar but unexposed rocks, plus an additional 107 cu. miles. Interestingly, more than half of Kilimanjaro's volume is represented by older, basal basalts (672 cu. mi.), so once again- as in Cascade stratovolcanoes - a basaltic shield is the most important, but least conspicuous element of a chemically complex volcano. Kilimanjaro- Africa's largest volcano and among the largest on the Earth is indeed a beautiful and fascinating volcano of the world.
Sources of information: Richard, J.J., Neumann van Padang M., 1957, Africa and the Red Sea. Catalog of Active Volcanoes of the World, Rome: IAVCEI 4, p.75-78.
Dr. Charles A. Wood, Volcano World
The Geology of Kilimanjaro 1972; by C. Downie & P. Wilkinson
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