Answer:
People live close to volcanoes because Geothermal energy can be harnessed by using the steam from underground which has been heated by the Earth's magma.Apart from the volcano itself, hot springs and geysers can also bring in the tourists. This creates many jobs for people in the tourism industry.
Answer:
The Geologic Time Scale is a system of chronological measurements that relates to the study of rock and layers.
While the human time scale is the portion of the pedogenic time scale that covers periods of centuries, decades, or less.
Explanation:
Answer:
Here are the list...
Explanation:
Community Colleges
Borough of Manhattan Community College
Bronx Community College
Guttman Community College
Hostos Community College
Kingsborough Community College
LaGuardia Community College
Queensborough Community College
4-Year Colleges
Baruch College
Brooklyn College
City College of New York
College of Staten Island
Hunter College
John Jay College of Criminal Justice
Lehman College
Medgar Evers College
New York City College of Technology
Queens College
York College
Honors College
CUNY William E. Macaulay Honors College
Graduate Colleges
CUNY Graduate Center
CUNY Graduate School of Journalism
CUNY School of Law
CUNY School of Medicine
CUNY School of Professional Studies
CUNY School of Public Health
State University of New York
Fashion Institute of Technology
SUNY College of Optometry
SUNY Downstate Medical Center
SUNY Empire State College (The Harry Van Arsdale Jr. Center for Labor Studies)
SUNY Maritime College
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Answer:
D. Seafloor bedrock is younger near the ridge and older farther away.
Explanation:
In a divergence boundary oceanic plates or continental plates move apart. The plates moves apart causing an uprising of molten magma to form a new crust. The divergent movement of plate is very prevalent in the oceanic plates.
The plates in the oceanic crust moves apart due to the up welling of aesthenosphere materials . These aesthenosphere materials(molten magma) are introduce to the ocean floor through the mid oceanic ridge . As this materials are introduced through cracks and fissures, the plates continue to drift apart. The molten magma later solidified to form a new crust closer to the oceanic ridge. This is why sea floor bedrock closer to the ridge is younger as new rocks are formed here. But as one move farther away from the ridge the rocks become older. This phenomenon provide ample evidence that the seafloor is spreading. The older rocks found father away from the ridge proves the seafloor has been spreading given way for new rocks closer to the ridge.
