1. plate boundaries using google earth. download the google earth file dynamic earth, it will outline the different plate boundaries. open google earth and go to file -open and choose the dynamic earth file. if you expand the file you'll see that there are several layers that you can turn on and off. for this activity you may want to turn off the seafloor age, volcanoes and earthquake layers. use the latitude/longitude coordinates given in the table below to determine the type of plate boundary at each location. these coordinates also match up with the descriptions in the table. type (or copy/paste) the coordinates into the search box in google earth and match up the locations and the geologic features/events to one of the listed plate boundaries. you may have to zoom out in order to see the location from the right perspective. each letter may be used > once. a. ocean-ocean convergent boundary b. ocean-continent convergent boundary c. continent-continent convergent boundary d. divergent boundary e. transform boundary latitudelongitude typ of la type of plate boundary latitude/longitude plate boundary 35.909 s, 72.733°w 27.988°n 86.925°e 38.322 n 142.369 e 4.00°s 12.24°vw 46.191°n 122.194°w 11.329°n, 142.206 e the deepest point on 35.900 n 120.433w earth the deepest point on earth san andreas fault highest point on earth 2011 japan 9.0 earthquake epicenter mt. st. helens, a well- known active volcando mid-atlantic ridge 2101 chile 8.8 earthquake epicenter

most historians agree that gabriel mouton, the vicar of st. paul’s church in lyons, france, is the “founding father” of the metric system. he proposed a decimal system of measurement in 1670. mouton based it on the length of one minute of arc of a great circle of the earth (now called a nautical mile, 1852 meters). he also proposed the swing-length of a pendulum with a frequency of one beat per second as the unit of length (about 25 cm). a pendulum beating with this length would have been fairly easy to produce, thus facilitating the widespread distribution of uniform standards. over the years, his work was revised, improved, and extended by a number of french scientists.

the political sponsor of weights and measures reform in the french revolutionary national assembly was the bishop of autun, better known as talleyrand. under his auspices, the french academy appointed several committees to carry out the work of developing a usable system of weights and measures for france. one of the committees recommended a decimalized measurement system based upon a length equal to one ten-millionth of the length of a quadrant of the earth’s meridian (i.e., one ten-millionth of the distance between the equator and the north pole).

the correct answer would be b. amelia, because the particals of gas move really fast (charged particals) and gas also has a lot of room (particals move independently) so the only answer that has both of those is amelia's.

alchemy hadn't scientific methods of study, appeal to mysticism and fantasy, the knowledge of chemistry and physics were modest at that time.

alchemy was - but as new rules were discovered it either changed into chemistry or it became "unscientific".