what kind of metamorphism occurs next to an intrusion of molten magma?
I think you have problems, non of wich is weight related.
It varys for different peopleI was 111 at the beginning of track and, two weeks later, I was down to 105You also have to eat healthy tooStart by walking around your neighborhood or down at the parkThen when you think you are ready, start jogging.
4 lbs is water weight! It's nothing, try eating at a minimum for 1 week, you'll lose it! and well, if you want to lose more, you'll have to sweat it out, go to the gym or run! steam room and spa helps me a lot toobest workout is in the morning!
well if your really desperate use weight loss pills, but if your not try some excserise , by a dog and walk it every day i guarentee you'll lose a few poundsmaybe not 10 but 4 or 3 would be enoughi bet your not even fat, so stop looking at urself in a negative way, accept who you are? who cares whhat people think.
It's called contact metamorphism, sometimes also called thermal metamorphism (but whichever name you use, it's the same thing)Contact metamorphism occurs in country rock, which is basically the large scale rock that was already living there happily before the igneous intrusionThese rocks become baked into what is called a ceramic form due to heat escaping from the intrusion, and which also comes with very hot hydrothermal fluidsIn this case, pressure is not a significant factor (unlike Barrovian metamorphism)Since there is little to no pressure, you won't end up with a foliated rockSoinstead of something like a slate or a schist with foliation (kind of like layers), you'll get a granular rock (hornfels)This type of metamorphism generally leads to localized alteration of the rock, because the thermal energy is not conducted will through the country rock (i.eit's a good insulator of the igneous intrusion)This can lead to extremely complex cases where a larger-scale form of metamorphism will come in and metamorph the metamorphmeaning that we really have to put boots on the ground to figure out the geologic history of the area.
