The Owner of the WLAN Patent One key patent for Wi-Fi technology that has won patent litigation lawsuits and does deserve recognition belongs to the Commonwealth Scientific and Industrial Research Organisation of Australia.
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In 1992 the first Australian WLAN patent was filed for, the US patent was filed for in 1993 and approved in 1996. This led to the creation of prototypes and the founding of Radiata Inc by Dave Skellern and Neil Weste from Macquarie University. They took out a non-exclusive patent on the technology from CSIRO in 1997.
Sunderbans forests, locally known as Badabon, are one of the richest biodiversity hotspots in India. This UNESCO World Heritage site is known for its mangroves, coastal forests that serve as a biological buffer between the land and sea.
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With its high levels of plant and animal endemism, and limited remaining natural habitat, Indo-Burma ranks among the top 10 biodiversity hotspots for irreplaceability and the top five for threat. The future of much of Indo-Burma’s ecosystems and species hangs in the balance.
Listed as one of the world’s “megadiverse” countries and sustaining close to 10 per cent of the planet’s biodiversity, Colombia ranks first in bird and orchid species diversity and second in plants, butterflies, freshwater fish and amphibians.
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A WiFi hotspot is a wireless access point that you can connect to to use Internet connection. WiFi hotspots work just as your WiFi router does at home by providing wireless connection to the users in the covered range.
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A volcanic “hotspot” is an area in the mantle from which heat rises as a thermal plume from deep in the Earth. High heat and lower pressure at the base of the lithosphere (tectonic plate) facilitates melting of the rock.
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Although Hawaii is perhaps the best known hotspot, others are thought to exist beneath the oceans and continents. More than a hundred hotspots beneath the Earth’s crust have been active during the past 10 million years.
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A frequently-used hypothesis suggests that hotspots form over exceptionally hot regions in the mantle, which is the hot, flowing layer of the Earth beneath the crust. Mantle rock in those extra-hot regions is more buoyant than the surrounding rocks, so it rises through the mantle and crust to erupt at the surface.
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Two prominent hotspot tracks appear on a map of the 50 United States, one involving a plate with thin oceanic crust (Hawaii), and one with thicker continental crust (Yellowstone).
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Hotspots. Hotspots are places where the magma rises up through the crust. They are caused by a static source of magma, often away from plate margins. As the plate moves away from the hotspot, a new volcano island will form.
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Hotspots occur when one of the Earth’s plates moves over an unusually hot part of the Earth’s mantle. These hot areas are usually relatively stationary and result in large amounts of magma rising up, piercing a hole in the plate to form a volcano. As the plates move, a series of volcanoes can form.
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A hotspot forms when a plume of magma rises from the mantle and melts through whatever crust is above it. This new magma tries to reach the curface and creates a volcano. But when the tectonic plate shifts, new crust is suddenly above the hotspot, and a new volcano forms. This is how hotspot volcanoes form.
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Hotspots are stationary magma plumes deep in the Earth that create volcanoes on the surface (eg Mount Kilauea in Hawaii). On a hotspot, magma comes to the surface through cracks in the rocks with great heat and low pressure. Hotspots can be linked to plate margins or may just form on a crustal plate.
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A hot spot is an area on Earth over a mantle plume or an area under the rocky outer layer of Earth, called the crust, where magma is hotter than surrounding magma.
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This upwelling of molten rock, known as a “hot spot,” creates volcanoes that spew out lava (magma that reaches Earth’s surface). The lava then cools and hardens to create new land. The Hawaiian Islands were literally created from lots of volcanoes”they’re a trail of volcanic eruptions.
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Hot spots are found around the globe, on land and in the ocean. The Hawaiian Islands are the youngest volcanic mountains in a long chain of volcanoes that formed over a hotspot.
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These so-called “hotspot” volcanoes are created when a narrow stream of hot mantle rises up from deep inside the earth and melts a hole in the plate so that the magma can ooze upward. The Hawaiian islands, for example, are a result of hotspot volcano formations near the center of the giant Pacific plate.
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A volcanic “hotspot” is an area in the mantle from which heat rises as a thermal plume from deep in the Earth. High heat and lower pressure at the base of the lithosphere (tectonic plate) facilitates melting of the rock. This melt, called magma, rises through cracks and erupts to form volcanoes.
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hot spot. A volcanic region that is fed by a hot plume of magma in the mantle where magma generated by the plume rises through the rigid plates reaching Earth’s surface. plume.
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Volcanic activity at hot spots can create submarine mountains known as seamounts. Some scientists estimate that seamounts make up 28.8 million square kilometers (17.9 million square miles) of the Earth’s surface, an area larger than any other habitat.
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The ‘ring of fire’ is a group of volcanoes that are located along the plate margin of the Pacific plate. Hawaii is an arc of volcanic islands, found above a hot spot.
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A hotspot is a large plume of hot mantle material rising from deep within the Earth.
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An island chain is formed when Earth’s plates move over a hot spot. Magma is pushed through the plate and creates an underwater volcanic mountain. The mountain grows and forms an island.
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The lava cools down and forms a volcano. The hot spot itself never changes position, but the tectonic plates are constantly moving, so the volcano formed will “move” along with the tectonic plate to the direction where ever the tectonic plate is heading, but at the same time the hot spot doesn’t stop producing lava.
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Hot spots are mantle plumes, which are columns of hot magma rising through the mantle until it reaches the crust. The plume burns its way through the crust due to convection. This forms Shield volcanoes which typically have gentle slopes and runny lava. The plates move over the hot spot.
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Hotspot. A small area of the Earth’s crust where an unusually high heat flow is associated with volcanic activity, A weak spot in the middle of a tectonic plate where magma surfaces; forms a volcano.
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Anywhere on a tectonic plate. They are RARELY found at plate boundaries.
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Volcanoes form when magma , molten rock from the mantle, reaches the Earth’s surface. The magma erupts to form lava at the surface, either on land or under the sea. Volcanoes usually form along plate margins , where crustal plates are either moving towards or away from one another.
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A volcano is an opening in the Earth’s crust that allows magma, hot ash and gases to escape. Volcanoes can look like mountains or small hills, depending on what type they are. Magma is molten rock ” rock that is so hot it has turned into liquid.
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Earthquakes are found at all three plate boundaries: constructive, destructive and conservative plate boundaries.
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As the volcano erupts, they build up layers of lava that may eventually break the water’s surface. When the tops of the volcanoes appear above the water, an island is formed.
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The Hawaiian Islands were formed by such a hot spot occurring in the middle of the Pacific Plate. While the hot spot itself is fixed, the plate is moving. So, as the plate moved over the hot spot, the string of islands that make up the Hawaiian Island chain were formed.
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Examples include the Hawaii, Iceland, and Yellowstone hotspots. A hotspot’s position on the Earth’s surface is independent of tectonic plate boundaries, and so hotspots may create a chain of volcanoes as the plates move above them.
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A frequently-used hypothesis suggests that hotspots form over exceptionally hot regions in the mantle, which is the hot, flowing layer of the Earth beneath the crust. Mantle rock in those extra-hot regions is more buoyant than the surrounding rocks, so it rises through the mantle and crust to erupt at the surface.
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Volcanoes usually form along plate boundaries , where tectonic plates are either moving towards or away from one another: Constructive boundary (or divergent boundary) ” this is where two plates move away from one another. Magma rises up to fill the gaps between the plates usually to create a shield volcano .
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A volcano is formed when hot molten rock, ash and gases escape from an opening in the Earth’s surface. The molten rock and ash solidify as they cool, forming the distinctive volcano shape shown here. As a volcano erupts, it spills lava that flows downslope. Hot ash and gases are thrown into the air.
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Most tsunamis are caused by earthquakes at destructive plate boundaries . Here, an oceanic plate is subducted into the mantle beneath a continental plate. This movement causes friction, which in turn causes the plates to stick. Energy accumulates, like that of a compressed spring.
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Pressure builds up inside the Earth. When this pressure is released, eg as a result of plate movement, magma explodes to the surface causing a volcanic eruption. The lava from the eruption cools to form new crust. Over time, after several eruptions, the rock builds up and a volcano forms.
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On land, volcanoes form when one tectonic plate moves under another. Usually a thin, heavy oceanic plate subducts, or moves under, a thicker continental plate. When this happens, the ocean plate sinks into the mantle.
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A supervolcano is a volcano on a massive scale. It is different from a volcano because: it erupts at least 1,000 km 3 of material (a large volcano erupts around 1 km 3) it forms a depression, called a caldera (a volcano forms a cone shape) a supervolcano often has a ridge of higher land around it.
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Earthquakes occur when tension is released from inside the crust. Plates do not always move smoothly alongside each other and sometimes get stuck. When this happens pressure builds up. When this pressure is eventually released, an earthquake tends to occur.
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An earthquake is a sudden shockwave caused by rocks being under stress from the movements of plates at plate boundaries. Eventually the stress in the rock builds up enough to deform and reach breaking point. At that point, the stored up energy is released in the form of shockwaves.
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It is solid and made up of iron and nickel with temperatures of up to 5,500°C. The outer core is the layer surrounding the inner core. It is a liquid layer, also made up of iron and nickel. The mantle is the thickest section of the Earth at approximately 2,900 km.
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Hotspots. Hotspots are places where the magma rises up through the crust. They are caused by a static source of magma, often away from plate margins. As the plate moves away from the hotspot, a new volcano island will form.