The graph shows calculations for potassium-argon dating. Potassium Argon Dating graph. The x axis is Billions of Years in increments of 1.3. The y axis is Remaining Portion of Potassium, measured in fractions starting at StartFraction 1 over 16 EndFraction, each entry double the previous one. 0 Billions of Years, StartFraction 1 over 1 EndFraction. 1.3 Billions of Years, StartFraction 1 over 2 EndFraction. 2.6 Billions of Years, StartFraction 1 over 4 EndFraction. 3.9 Billions of Years, StartFraction 1 over 8 EndFraction. 5.2 Billions of Years, StartFraction 1 over 16 EndFraction. Which statement explains what geologists can learn from the graph? They can estimate that all the potassium will have decayed within 6.5 billion years. They can tell that 1/8 of the argon gas will be left after 3.9 billion years. They can determine that a rock is 1.3 billion years old if 1/2 of the potassium has decayed. They can see that potassium’s half-life varies from every 1.3 billion years to every 5.2 billion year

you go to appeals court like section e

i would think yes.

explanation:

because we have every natianlity in our country which makes us so diverse and unique. that's why in a lot of cities there are places like little italy, koreatown, chinatown.  

the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)