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The map below shows the area that, at one time, was covered by ancient Lake Bonneville. Evidence of ancient shorelines indicates that, near the end of the last ice age, Lake Bonneville existed in western Utah and eastern Nevada. The Great Salt Lake in Utah is a remnant of the former Lake Bonneville.
Which material that was formerly on the bottom of Lake Bonneville is most likely exposed on the land surface today?
(1) folded metamorphic bedrock
(2) flat-lying evaporite deposits
(3) coarse-grained coal beds
(4) fine-grained layers of volcanic lava

The map below shows the area that at one time was covered by ancient Lake Bonneville Evidence of ancient shorelines indicates that near the end of the last ice class=

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metchelle
The correct answer for the given question above would be option 2. Based on the given description above about the history of  Lake Bonneville, the material that was formerly on the bottom of Lake Bonneville that is most likely exposed on the land surface today would be a flat-lying evaporite deposits. Hope this answers your question.

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