Arrange the tiles to show the sequence of events in the development of the theory of evolution. darwin collected specimens from around the world during the hms beagle voyage. darwin proposed the theory of evolution by natural selection. scientists collected fossils that showed species changing over time. scientists examined evolutionary relationships using dna sequencing. mendel proposed laws for how traits are inherited. ↓ ↓ ↓ ↓

Scientists collected fossils that showed species changing over time.  Darwin collected specimens from around the world during the HMS Beagle voyage.  Darwin proposed the theory of evolution by natural selection. Mendel proposed laws for how traits are inherited. Scientists examined evolutionary relationships using DNA sequencing.

Explanation:

Scientific knowledge does not remain the same over the years. What is considered true today may not be in the future or may be used as a basis for further studies. This evolution of scientific knowledge was extremely important and allowed science to reach the point we know and make our lives easier.

An example of this is the scientific evolution that allowed scientists to sequence DNA, helping to unravel many processes in the human body and find causes and treatments for various diseases. If we summarize this evolution, we can cite the following steps:

Scientists collected fossils that showed species changing over time.  Darwin collected specimens from around the world during the HMS Beagle voyage.  Darwin proposed the theory of evolution by natural selection. Mendel proposed laws for how traits are inherited. Scientists examined evolutionary relationships using DNA sequencing.

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.

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