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The mid-ocean ridge is a volcanic feature caused by the spreading apart of oceanic plates as part of plate tectonics, and is initially formed as a result of changes in the convection currents which seek the least resistant point to the surface. The sea floor at the ridges are uplifted by rising magma. The rising magma is part of a process of heat transfer from the interior of the Earth to the surface known as a convection current. As the rising magma cools, it forms new crust which becomes part of the ridge.
Hot spots and mid-ocean ridges are both geologic features associated with volcanic activity. Hot spots are stationary points of intense volcanic activity on the Earth's surface, whereas mid-ocean ridges are underwater mountain ranges formed by tectonic plates pulling apart. Both hot spots and mid-ocean ridges erupt magma from the Earth's mantle, creating new land or seafloor.
Mid-ocean ridges are underwater mountain chains where tectonic plates move apart, allowing magma to rise up and form new crust, often accompanied by volcanic activity. Seamounts are submarine volcanoes that are formed by lava rising from the ocean floor. Both mid-ocean ridges and seamounts are related to volcanic activity as they involve the release of molten rock (magma) onto the ocean floor.
High spots formed as new seafloor is created are known as seamounts or underwater mountains. These features are often formed by volcanic activity or tectonic movement along mid-ocean ridges. Seamounts can vary in size and shape, with some rising thousands of feet from the ocean floor.
This act is typically referred to as "emergence," where something rises or appears from a lower place or depth. It can also be described as ascension or rising to the surface.
The word "incense" appears on page 117 of the book "Esperanza Rising" by Pam Muñoz Ryan.
The mid-ocean ridge is a volcanic feature caused by the spreading apart of oceanic plates as part of plate tectonics, and is initially formed as a result of changes in the convection currents which seek the least resistant point to the surface. The sea floor at the ridges are uplifted by rising magma. The rising magma is part of a process of heat transfer from the interior of the Earth to the surface known as a convection current. As the rising magma cools, it forms new crust which becomes part of the ridge.
Hot spots and mid-ocean ridges are both geologic features associated with volcanic activity. Hot spots are stationary points of intense volcanic activity on the Earth's surface, whereas mid-ocean ridges are underwater mountain ranges formed by tectonic plates pulling apart. Both hot spots and mid-ocean ridges erupt magma from the Earth's mantle, creating new land or seafloor.
Mid-ocean ridges are underwater mountain chains where tectonic plates move apart, allowing magma to rise up and form new crust, often accompanied by volcanic activity. Seamounts are submarine volcanoes that are formed by lava rising from the ocean floor. Both mid-ocean ridges and seamounts are related to volcanic activity as they involve the release of molten rock (magma) onto the ocean floor.
Mid-ocean ridges are a line of volcanic mountains under the oceans between the continents. As the oceanic plates are being pulled apart by the processes of plate tectonics, magma is formed from decompression melting in the mantle, and rises upward to fill in the gap that is created.
Japan is often referred to as the "Land of the Rising Sun." This nickname comes from the Japanese word "Nihon" or "Nippon," which means "origin of the sun." The country is also known as the Land of the Rising Sun due to its location to the east of Asia, where the sun appears to rise first.
These are called divergent plate boundaries marked by ridges, caused by the uplift of crust by rising magma, on either side of a rift valley, where the magma fills in the gap left by the spreading ridges.
At mid-ocean ridges, new oceanic crust forms through the process of seafloor spreading. Magma rising from the mantle solidifies at the ridges, creating new crust as the tectonic plates move apart. This process results in the formation of basaltic rock and volcanic features such as pillow lava and hydrothermal vents.
The mid-ocean ridge is the Earth's longest continuous mountain range, approximately 55-65 thousand kilometers long and bilaterally divided by a valley called a rift. The mid-ocean ridge is a volcanic feature caused by the spreading apart of oceanic plates as part of plate tectonics. The sea floor at the ridges are uplifted by rising magma. The rising magma is part of a process of heat transfer from the interior of the Earth to the surface known as a convection current. As the rising magma cools, it forms new crust which becomes part of the ridge. Therefore, the ridge is composed of basalt and gabbro, and is among the most recent of geologic age crustal rock. :)
There are five so-called "Hannibal" movies. Frankie Faison appears in four of them: Manhunter, Silence of the Lambs, Hannibal and Red Dragon. He is Lt. Fisk in Manhunter and Barney Mathews in the remainder. None of the actors in the first four movies appears in the fifth movie, Hannibal Rising.
they are formed from the uplift of newly formed oceanic crust by rising magma.
they form in three main places where lithospic plate pull apartat mid-ocean ridges,where plates come together and making it thicker amd allowing to melt,see more at About Volcanism.