nowhere! because they don't exist!
during summer the sea make land cool because the hot air of land flow towards the sea from the sea the cool air flow toward land which makes it cool. this process known as land breeze and sea breeze
Mantle plumes result in the formation of hot spots.
the mantle is made up of solid hot rock.
Earths mantle is less dense and very hot. The mantle is 2885km thick.
area between the mantle and the core where hot rock is forced into the crust
the islands of hawaii
hot stuff rises, cool stuff sinks
The term hot spot is used to describe a very long-lived magma source located deep in the mantle. J. Tuzo Wilson is credited with having originated the concept of hot spots.
Magma in the mantle moves in a current called a convection current. A convection current is a circular flow of a substance in which a hot substance rises, cools, sinks, gets hot again, and repeats. In this way, magma in the mantle flows in currents of more hot or more cool magma.
The flow of mantle effects convection currents in the mantle. This process happens as hot material within the mantle begins to rise. As it rises, it begins to cool and then sinks. This process repeats as a cycle of convection currents.
Mantle plumes
The part of the tectonic plates located above mantle plumes are called "hot spots". --- Source(s) : Does Google count?
Volcanoes located at hot spots form by lying directly above columns of hot rock that rise through Earth's mantle. As a tectonic plate moves over a mantle plume, rising magma causes a chain of volcanic islands to form.
The layer of the Earth above the core is called the mantle. It is located between the core and the Earth's crust. The mantle is composed of hot, semi-solid rock.
A mantle is a layer of hot rocks.
Subduction results from convection in the asthenosphere. The heat from the core of the earth that is imparted to the mantle causes the mantle to convect much the wayboiling water convects in a pan on the stove. Hot mantle at the core-mantle boundary rises while cool mantle sinks, causing convection cells to form.
The mantle is the hot rock.