Estuaries are wetlands that form near the mouths of rivers along ocean coastlines. many trees fail in estuaries, but mangroves are an exception. mangroves are common in tropical estuaries, especially the everglades of southern florida. they thrive in the everglades because they tolerate much greater salinity levels than other plants do. they also have prop roots that support their weight in the everglades soil. the soil is wet and spongy, and often is covered in water. while the adaptations of mangroves are ideal for the everglades, they are less useful for other tropical regions, such as tropical rain forests. they can survive in these regions, but are less common there. the evidence in the passage most strongly supports which of these explanations of the range of mangroves? a. mangroves depend on relatively warm temperatures. b. mangroves depend on water of relatively high salinity. c. other trees outcompete mangroves in low-salinity environments. d. other trees outcompete mangroves in high-salinity environments.

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.