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 gevserite travertine limestone dripstone feldspar Surface runoff or a stream (river) that disappears into a joint of a sinkhole in a Karst topography is called a sink river. swallow hole. disappearing stream. hot spring. pillar. The primary substance that results from the two main dissolution processes o f 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 o l the following is NOT required to form Karst features? Water Limestone rich m 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 differenc

Explanation / Answer

Question no.7 Answer is (a)geyserite.

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