I think the difference in temperature can cause convection currents, because like the lava lamp the more hot something is the more dense it becomes then it rises to the top, the more cool something gets the less dense it becomes and it sinks to the bottom. So when plate tectonics go through a convergent boundary it slides under the crust it then has a current, which is caused from convection. Which then spreads. Then it heats up, and rises to the top. Once it 's at the top it cools down and becomes less dense then this process is repeated. An example of this is in a lava lamp, once the lava on the bottom of the lava lamp heats up it becomes more dense and rises to the top where there 's less heat, then they 're it cools down and sinks to the bottom this. …show more content…
Process happens over and over again to create the soothing satisfying effect of a lava lamp that we keep in our bedroom. like this cool room decor decoration, tectonic plates do the exact same thing. Except the heat from the mantle causes convection currents which is all a cycle. Relating back to the claim, Does temperature does cause convection currents, without it doing that that it wouldn 't be a cycle, so since heat is a form of temperature. Temperature does cause convection currents. Another example of convection currents is when we put two types of colored water in a vial, opened the cap of the vial and saw how it rose to the top. When we tested it with hot water it went straight up like a volcano, and settled at the top not mixing in with the regular temperature water
- Crust - cool, lightweight, brittle, which floats on top of mantle. It is the outer layer of earth. Tectonic processes reshape continents and also cause earthquakes - Tectonic plates- plates caused by convection currents in the mantle that causes earthquakes. - Ocean basins form where continents crack and pull apart. - Magma – is molten rock
The rock cycle is extremely helpful and useful for scientists all over the world. These scientists use physical geology, which carefully focuses on how rocks form into other rocks (Doc. 2). Also, through the rock cycle, three types of rocks form, which are called igneous rock, sedimentary rock, and metamorphic rock (Doc. 1). The rock cycle is much like the water cycle, but it takes millions of years for a rock to form, wear down, and form again. Also, scientists need the rock cycle to watch how the rocks form overtime (OI).
The Connecticut river valley was also formed from many rifts and faults that had developed. A rift valley is a region of lowland that forms where tectonic plates move apart, which is how the river valley was formed. On the other hand, the plate tectonics also formed the Appalachian mountains. The Appalachian mountains were formed by convergent boundaries, which is when two plates collide. The
Usually because the plates have friction, the stresses build up on the surface. The process is relatively slow with a rate of 1 inch per year, until one of the surface slips due to high pressure. The slippage speed up to 5000 miles an hour, the pressure tears down the fault to a stuck patch which slows down the speed of the moving plates. The plates may break though the stuck patch and continue to the next knot and affecting more area.(USGS) Geology in San
In general, volcanic activity related to subduction in oceanic and continental arcs seems to be caused by the melting of the mantle wedge above the subsiding lithosphere. A process which is induced by the release of hot fluids, essentially water (dehydration), by the descending slab into the asthenospheric wedge resulting in a decrease of the wedge's melting point often followed by its partial melting (4,5). Prior to the 1980 eruption, Mount St. Helens had been in a dormant state since 1856, having over the past 4 millenia displayed sporadic eruptive activity, seemingly increasing in frequency, with initial eruptions being separated by dormant intervals ranging from thousands to several hundreds of years to more recent intervals of 1 or 2 centuries in length
According to the theory of plate tectonics, the San Andreas represents the transform boundary between two major plates of the Earth’s crust: the Northern Pacific to the south and west and the North American to the north and east. The Northern Pacific plate is sliding laterally past the North American plate in a northerly direction, and hence the San Andreas is classified as
Volcanoes contribute geographically in the re-formation of the earth 's surface where the new rock layers arise as a result of hardened lava surging form a new terrain. In addition, they contribute to the emergence of new hot springs or what is known as hot baths. As the volcanic ash helps to enrich the ground soil, also people can take advantage of the volcanic rocks in the construction. Finally, the minerals that come out from the volcanoes have global economic value, which is a source of income of many
When temperature is increased, the amount of obtainable energy increases; meaning that particles will move at faster pace at a higher temperature. Thus rate at which molecules diffuse will progressively speed up as the temperature increases. However if temperature of solution is decreased the rate of osmosis will decrease and rate at which molecules diffuse will be significantly less than that of higher
The cooled air over the land moves in to take the place of the rising warm air over the water. That is how bodies of water can affect the
The two tectonic plates associated with Popocatepetl are the North American Plate, which is a continental plate and the Cocos Plate, which is a oceanic plate. These two plates move towards each other, this is known as convergence. The North American Plate and the Cocos Plate collided and Cocos
These two plates push and shove each other causing small tremors throughout which can cause landslides,volcanic eruptions and once in a couple years, quakes with devastating results. The strongest earthquake recorded occurred in 1991 with a measure of 7.6 on the Richter scale. This earthquake left 4 dead and buildings as well as bridges and road were completely destroyed. If another Earthquake occurs, the coastal cities would be the most affected ones as they are closer to the plates.
Heat stress is a condition in which the increase in core body temperature overwhelms the body’s homeostatic thermoregulation abilities, thus producing and absorbing more heat than the body could dissipate [1]. This results in a wide spectrum of heat-related illnesses, ranging from minor conditions such as heat cramps and heat exhaustion to the more severe condition known as heat stroke. Heat stroke is defined as a core body temperature of beyond 40.60C, commonly associated with the dysfunction of the Central Nervous System (CNS) and the failure of multiple organ systems, which may ultimately result in disability or death. [2] Heat stress can be categorized into two different entities: classical and exertional. Classical or environmental heat
Because hot material near the Earth's core rises, and colder mantle rock sinks. “It's kind of like a pot boiling on a stove. The convection drive plates tectonics through a combination of pushing and spreading apart at mid-ocean ridges and pulling and sinking downward at subduction zones.” Scientist Van der Elst said. Before people
Earthquakes and waves pushed the supercontinent apart, showing how strong that tectonic plates can be. Although the oldest human fossil could be up to one million years old, scientists are still unaware
Earthquakes are caused when rock underground suddenly breaks along a fault. This sudden release of energy causes the seismic waves that make the ground shake. When two plates are rubbing against each other, they stick a little. Most earthquakes occur along the edge of the oceanic and continental plates. Due to stress they shift and cause the earthquake.