Yellowstone Park

The government systematically misled the public about the numbers of wolves that would be involved in the reintroduction into Yellowstone Park. The organization Defenders of Wildlife cited thirty-five to forty-five wolves as being the target numbers. 

Fournier (personal communication, 1974) feels that calcic montmorillonites will persist to higher temperatures. This opinion is based upon former (Honda and Muffler, 1970) and more recent work in Yellowstone Park,... 

Wyoming, including South Dakota and Yellowstone Park. 134... 

Scorodite,9 FeAs04.2H20, occurs as pale green or brown rhombic crystals of density 3 1 to 3 3 hardness 3-5 to 4. It owes its name (Greek skorodon, garlic) to the fact that, when heated, it emits the characteristic odour of arsenic. It occurs in Cornwall, and in a readily oxidisable form as a deposit from certain geysers in Yellowstone Park,10 U.S.A. A hydrated arsenate of iron and aluminium is known as Liskeardite.11... 

Geothermal fluids are a common agency for zeolite formation and this has been well documented in Iceland, at Wairakei (New Zealand), and in Yellowstone Park (USA). Often, well-defined zones (illustrated for Iceland in Figure 14)... 

Wilcox R. E. (1944) Rhyolite-basalt complex on Gardiner River, Yellowstone Park, Wyoming. Geol. Soc. Am. Bull. 55, 1047-1080. 

On a hike through Frijoles Canyon with the Fermis, Niels Bohr stopped to admire a skunk, an animal unknown to Europeans, but it chose not to instruct the vigorous Dane in the pungency of its defenses. Bears sometimes appeared on the trails, prompting warnings in the daily bulletin Remember that these are not tame bears like those in Yellowstone Park. ... 

Based on available geochemical data, in particular on the architecture of the ancient VMS deposits [105,261,265], one can envision networks of photosynthesiz-ing and habitable bands of precipitated ZnS and MnS around primeval hot springs. These networks of joined rings at the spots of geothermal activity, a kind of primeval Yellowstone Park realm, could represent the first Earth biotopes (see Fig. 2). 

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