Answer:
Carol Gilligan believed earlier researchers into morality had overlooked the perspective of females.
Explanation:
Gilligan was Kohlberg's reserach assistant, but argued that Kohlberg's stages of moral development were male-orientated. Therefore, these stages were limited in there ability to be generalized to females. Because of these, Gilligan proposed her theory of stages of female moral development.
Answer: They were tilted after they were deposited; they were originally deposited horizontally; the youngest layer was originally deposited as the bottom layer; their relative ages have not changed even though they are tilted.
Geologic tilting is the process by which the Earth's rock layers begin to slant irregularly. This can be caused by vertical or horizontal faults, <em>angular unconformity</em> and disturbances on the Earth's magnetic field.
A geologist cannot know the exact age of a rock layer just from looking at it. The information can only be obtained by other methods, to an approximation. He can, however, know that the youngest layer is the one that was originally at the bottom. He also knows that the relative age of the layers has not changed.
<em>Angular unconformity</em> occurs when a new layer of sedimentary rock is deposited on layers that were already tilted, thus exacerbating it. By looking at the layer carefully, the geologist can find out whether the tilting happened while the sediments were being deposited, or afterwards. He can also know which way they were originally deposited by studying characteristics such as cracks and ripple marks.
<u>Answer</u>:
When heat from inside Earth is transferred to its surface "More dense material is pushed to the crust".
<u>Explanation</u>:
The Earth is made of four different layers- crust, mantle, liquid outer core and solid inner core. Out of these, the inner core has the highest temperature. As heat moves from area of high temperature towards area of lower temperature, the heat from inner core transfers towards the outermost surface of the Earth i.e. crust which happens through conduction and convection. As the heat moves from the core towards crust, the materials around the inner core starts losing heat and hence become less dense and as the heat reaches the surface warm and more dense materials gets pushed to the crust in form of magma.
He painted the ceiling of the sistine chaple the last jugment
