What Is Not Likely To Happen At A Divergent Boundary - Web when a divergent boundary develops in continental crust, it has two consequences, one sedimentary and one igneous. Secondly, due to heat transfer to surrounding rock, you eventually loose so much energy that the magma crystalises (freezes). This means that the closer to the crust, the cooler it will be. Web the effect is twofold. Web divergent plate boundaries are locations where tensional forces are pulling things apart. In locations where lithospheric plates are diverging, the rates of divergent motion range from 2 to 17 cm/year. Firstly, temperature increases as preassure increases and preassure increases as depht increases. A fresh divergent boundary developing in continental lithosphere, east africa.
Web the effect is twofold. In locations where lithospheric plates are diverging, the rates of divergent motion range from 2 to 17 cm/year. Web when a divergent boundary develops in continental crust, it has two consequences, one sedimentary and one igneous. A fresh divergent boundary developing in continental lithosphere, east africa. Secondly, due to heat transfer to surrounding rock, you eventually loose so much energy that the magma crystalises (freezes). Web divergent plate boundaries are locations where tensional forces are pulling things apart. Firstly, temperature increases as preassure increases and preassure increases as depht increases. This means that the closer to the crust, the cooler it will be.