Light energy from the sun is the primary source for all living organisms. so how does the sun provide energy for all living organisms? in this assignment, you will explain how energy from sunlight is used during photosynthesis, then how the energy is transferred to animals that cannot harness energy directly from the sun.

your mission is to use your knowledge of photosynthesis and respiration to explain what happens during these processes and how energy is made and transferred.

presentation should include the following:

detailed descriptions of what happens during:
photosynthesis (the light-dependent reactions and the light-independent reactions)
transitioning between photosynthesis and respiration
cellular respiration or fermentation

an explanation of how the molecules in photosynthesis and cellular respiration are similar. include descriptions of the molecules involved in each of the processes above.

complete sentences should be used in all written descriptions and explanations
illustrations, diagrams, or images that explain the transition between the reactions of photosynthesis and cellular respiration.
you can create your own images, or use images from websites or other sources.
if you use premade images, you will need to give a reference of the source of that image and create your own unique caption to describe the image.
your presentation should be detailed and organized, but it can be presented in a variety of ways:

1.illustrated story
2.slide presentation
3.comic strip

Silicon is cut into tiny pieces for computer chipslead is melted to form pelletsliquid water freezes to form ice

Mantle convection  is the slow  creepingmotion of earth's solid silicate  mantle  caused by  convection  currents carrying  heat from the interior  to the planet's surface.[1][2]  the earth's surface  lithosphere, which rides atop the  asthenosphere  (the two components of the  upper mantle), is divided into a number of  plates  that are continuously being created and consumed at their opposite  plate boundaries. accretion occurs as mantle is added to the growing edges of a plate, associated with  seafloor spreading. this hot added material cools down by  conduction  and  convection  of heat. at the consumption edges of the plate, the material has thermally contracted to become dense, and it sinks under its own weight in the process of  subduction  usually at an  ocean trench.[3]this subducted material sinks through the earth's interior. some subducted material appears to reach the lower mantle,[4]  while in other regions, this material is impeded from sinking further, possibly due to a phase transition from  spinel  to  silicate perovskiteand  magnesiowustite, an  endothermic reaction.[5]the subducted oceanic crust triggers  volcanism, although the basic mechanisms are varied. volcanism may occur due to processes that add buoyancy to partially melted mantle causing an upward flow due to a decrease in density of the partial melt.secondary forms of convection that may result in surface volcanism are postulated to occur as a consequence of intraplate extension[6]  and  mantle plumes.[7]it is because the mantle can convect that the  tectonic plates  are able to move around the earth's surface.[8]mantle convection seems to have been much more active during the  hadean  period, resulting in gravitational sorting of heavier molten  iron, and  nickel  elements and  sulphides  in the core, and lighter  silicate minerals  in the  mantle.

Photo means light and synthesis means combination so combination of light