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 correct answer for the given question above would be option 2. Based on the given description above about the history of Lake Bonneville, the <span>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.</span>
Land controlled by Azerbaijan which can be rephrased as Nakhichevan and Ngorno-Karabakh regions which are exclaves each in the other respective country.
Particularly distinctive of the climate are sclerophyll shrublands, called maquis in the Mediterranean Basin, chaparral in California, matorral in Chile, fynbos in South Africa, and mallee and kwongan shrublands in Australia