Answer:
a) divergent boundaries by submarine eruptions and intrusions of basaltic magma
Explanation:
Divergent boundary is where tectonic plate move apart from each other. Divergent boundary is mostly prevalent in the oceanic crust. The opposing plate tends to move apart from each other.
On the oceanic crust plates move apart from each other causing an upwelling of magma from the aesthenosphere. This magmatic material is introduced through the oceanic ridges. As the magma are introduce the opposing plates separates further . The basaltic magma introduced through the oceanic ridges forms the new oceanic crust. As we move away from the oceanic ridge the rocks gets older . The oceanic ridge where the basaltic magma erupt depict the youngest rocks.
Answer:
Ummmmmmmmmmm
Explanation:
Brainliest I answered first
Answer:
<em>the next time they'll next toll together is 180 minutes.</em>
Explanation:
Time interval for tolling = 9 min, 12 min, and 15 min.
The next time they will toll together will be the LCM of their time intervals.
we find the LCM of the three numbers as shown below
LCM of 9 = 3 x 3 = 
LCM of 12 = 2 x 2 x 3 =
x 3
LCM of 15 = 3 x 5
we represent each factor with the factor with the highest power i.e
,
and 5
the LCM is then =
x
x 5 = 180
<em>the next time they'll next toll together is 180 minutes.</em>
Answer:
1.stonehenge
Parthenon
Mount rushmore
Taj Mahal
Great pyramid of giza
Miami statues
Machu picchu
The roman colosseum
The leaning tower of pisa
Great wall of china
Georgia guidestones
The fork
Cadillac ranch
Fallen angel square
Hand of desert
They are made of granite, marble and bronze.
I hope this helps