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:
The correct options are: a. the number of additional neutrons of an isotope is too large; d. the number of additional neutrons of an isotope is too small
Explanation:
The chemical elements that have the same number of protons in the nucleus but different number of neutrons are known as isotopes. Isotopes can be stable or unstable.
The isotope having an unstable nucleus, due to the presence of additional neutrons in the nucleus of the atom, is known as a radioisotope.
Also, chemical elements that have atomic number greater than 83 have unstable nuclei and thus they are called radioisotopes.
Answer:
I don't know precisely but the distance from the equator to the pole is 10,000 km
This province has several subprovinces, including the active and sometimes deadly volcanoes of the Cascade Range and the young, steep mountains of the Sierra Nevada. The rocks that form the backbone of the Sierra Nevada are mostly granitic rocks that formed during the Mesozoic Era, when dinosaurs roamed the Earth.
Strong winds, I think! :)
