Answer: The Turquoise Lake as seen nowadays in Colorado is a result of the 1850´s modern warming climate transition, lingering away from the Little Ice Age times occurred 500 years ago. This given period was characterized by snow blowing winds that accumulated ice through thermal compaction, generating the glaciers as we see them.
Explanation: Terminal and recessional moraines are the terminus of a glacial feature. Moraines are the sedimentar charges carried by melted glacials. Consequence of those is the repositioning of the snow downwards the valleys. The ice, initially attached to the glaciers and mountain tops, undergoes melting by seasonal and/or climate transition warming, resulting on circumstancial water deposits that place on the basin/lower areas of the mountain chains, forming lakes.
Answer: <em>Mean sea level is an average level of the surface of one or more of Earth's bodies of water from which heights such as elevation may be measured.</em>
A topographic map uses contour lines to show elevation
Answer:
Matterhorn Mountains in Switzerland
Explanation:
The popular Matterhorn Mountains in Switzerland experiences three forms of glacial erosion: Cirques are formed when glaciers deplete the mountainside, scour it and create circular holes with steep uphill faces, designed like inverted bowls. Mountains grow when movements of the Earth's crust push the rocks up.
Answer: 46° N, 30° E
Explanation: Odessa is one of the most wonderful coastal city of Ukraine with Latitude and longitude coordinates 46° North and 30° East.
It is known for its beaches and 19th-century architecture, including the Odessa Opera and Ballet Theater. It has an Area of 162.4 km² with population of about 993,120 .
Odessa hosts both the Port of Odessa and Port Yuzhne, a significant oil terminal situated in the city's suburbs. During the 19th century, Odessa was the fourth largest city of Imperial Russia, after Moscow, Saint Petersburg and Warsaw.