The silica-rich evaporate deposits that surround geysers in the Yellowstone Basi

Question

The silica-rich evaporate deposits that surround geysers in the Yellowstone Basin are made of a material called geyserite travertine limestone dripstone feldspar surface runoff or a stream (river) that disappears into a joint or a sinkhole in a karst topography is called sink river. swallow hole. disappearing stream. hot spring. Pillar. The primary substance that results from the two main dissolution processes of limestone is water carbon dioxide. calcium silicate. dolomite. calcium bicarbonate. The landform labeled A in Figure 2 is found in a karst topography is called inselberg conical hill earth mound mogotes (haystacks) plume Which of the following is NOT required to form Karst features? Water Limestone rich in calcium carbonate Fractures and joints in the rocks High wind Weathering by solution The following landforms may be found in a karst cavern except_____ underground stream stalactite Stalagmite mogote column The primary difference between stalactites and stalagmites is the _______ in a cavern location. age. chemical composition. height. travertine content. The widespread geyser activity at Yellowstone National Park is the result of a hot spring. Volcano. mountain building process. travertine terrace. Magma chamber underneath the surface. One of the common surface features of karst landscapes are sinkholes, also known as _______. travertine dripstone dolines tufa

Explanation / Answer

7. geyserite

8. disappearing stream

9. calcium bicarbonate

10. conical hill

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