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What else can I help you with?
How were dishes washed in the 1950?
with soap and water in a sink by hand with a dishrag, or by a special 1950's dish cleaning dog.
What time did the wahine sink?
the wahine sank because the captio did not pull out to sea much at all
What is the purpose of consumer rights?
I don't know if you can remove dye from the aeslant you may have to pick it off and re-seal.I have a white sink and use comet.
Who has the most power if there is a national emergency?
The President . It is obvious as he is commander-in-chief. by the way the Navy dept had a short lived and somewhat sardonic acronym for this role- CINCUS pronounced ( Sink-Us!) Commander In chief, US-) Only He can sink us! With regard to aquatic scandals such as the Watergate (Nixon) and Whitewater (Clinton) it may be an apt choice but was ditched in favor of Potus- President of The US. CINCUs may still be used but a well it might be considered washed-up.
Samuel Adams nicknames?
President John Adams had the following nicknames:The Colossus of Independence -- Given to him by Thomas Jefferson for his leadership in Congress in 1776The Duke of Braintree -- A sarcastic reference to his grandiose airsKing John the SecondOld Sink or Swim -- For the speech in which he vowed "To sink or swim; to live or die; survive or perish with my country"His Rotundity -- for being rather overweight and fond of formalThe Atlas of Independence
When does a part of oceanic plate sink into the mantle?
Usually when it meets another tectonic plate at a convergent plate boundary. If the oceanic plate converges with a continental plate the denser oceanic plate will be forced under the continental plate. If it converges with another oceanic plate the older (and therefore cooler and denser) plate will be forced under the younger plate.
Does the old oceanic plates sink into the mantle at mid-ocean ridges in a process called subduction?
No, old oceanic plates do not sink into the mantle at mid-ocean ridges; instead, mid-ocean ridges are the sites of seafloor spreading, where new oceanic crust is formed. Subduction occurs at convergent plate boundaries, where an older, denser oceanic plate sinks beneath a lighter continental plate or another oceanic plate into the mantle. This process helps recycle the oceanic crust and is responsible for the formation of features like deep ocean trenches.
What causes some oceanic plates to sink and others to float?
Oceanic plates sink because they are denser than the underlying mantle, due to cooling and becoming more compact over time. In contrast, other plates float because they are less dense than the mantle material below, allowing them to remain buoyant on top.
When an oceanic plate and a continental plate converge the oceanic plate subduct or sink below the continental plate because?
the oceanic plate is denser than the continental plate. As the two plates converge, the denser oceanic plate descends into the mantle at a subduction zone, leading to geological phenomena such as earthquakes and volcanic activity. This process also contributes to the formation of mountain ranges and oceanic trenches.
What ocean plate and continental plate colliding?
At this type of convergent boundary the oceanic plate will be subducted, or sink into the mantle underneath the continental plate. Volcanoes often form near these boundaries.
What is a rock plate that sinks back into the mantle called?
A rock plate that sinks back into the mantle is called a subducting plate. This process occurs at convergent plate boundaries where denser oceanic plates sink beneath lighter continental plates.
What happens to the oceanic plate as is descends below 700 km into the mantle?
As the oceanic plate descends below 700 km into the mantle, it undergoes increasing temperatures and pressures, which can cause dehydration and partial melting of the subducted material. This process leads to the release of fluids that can trigger volcanic activity in the overlying mantle. The plate continues to sink deeper, eventually becoming part of the mantle's convective flow, where it may contribute to mantle dynamics and the formation of new geological features. Over time, the plate may eventually be assimilated into the mantle, altering its composition and properties.
At deep ocean trenches what allows oceanic crust to sink back into the mantle?
Conduction. Heat istransferred from the mantle to the crust, melting it to become part of the mantle.
What kind of plate boundary cost old and heavy crust to sink in to the mantle?
A subduction zone is the plate boundary where old and heavy oceanic crust sinks into the mantle. At subduction zones, oceanic crust is forced beneath another tectonic plate, typically a continental plate, due to differences in density. This process can lead to the formation of deep oceanic trenches and volcanic arcs on the overriding plate.
What causes one plate to sink while another floats?
The phenomenon of one tectonic plate sinking while another floats is primarily due to differences in their density and composition. Oceanic plates are generally denser and thinner than continental plates, which are thicker and less dense. When an oceanic plate converges with a continental plate, the denser oceanic plate will subduct, or sink, into the mantle. This process is driven by gravitational forces and the dynamics of the Earth's mantle, leading to geological activity such as earthquakes and volcanic eruptions.
Why does plates sometime sink into the mantle?
Plates can sink into the mantle at subduction zones because the descending plate is denser than the underlying mantle. This happens because the oceanic crust of the descending tectonic plate is denser than the underlying mantle rock.
What does the ocean floor sink into the mantle?
The ocean floor sinks into the mantle primarily due to the process of subduction, where one tectonic plate is forced beneath another into the Earth's mantle. This usually occurs at convergent plate boundaries, where an oceanic plate collides with a continental plate or another oceanic plate. The denser oceanic crust is pushed down, creating trenches and leading to geological phenomena such as earthquakes and volcanic activity. This recycling process is a key component of the Earth’s lithospheric dynamics and plate tectonics.
