Put the events in order to show how a bill becomes a law. bill passes in both houses, president signs or vetoes the bill, bill is sent to the president, bill is introduced in congress.

1. Bill is introduced in Congress

2. Bill passes in both-houses

3. Bill is sent to the president

4. President signs or vetoes the bill

Explanation:

The U.S. Congress holds two legislative assemblies: the U.S. Senate and the U.S. House of Representatives. Anybody elected to either of them is entitled to propose a new law.

Once both houses have accepted a bill, they send it to the president, who then analyzes the bill and is able to approve it and sign it into law or veto it.

If the president chooses to veto a bill, Congress can decide to override that veto and the bill turns into a law. But, if the president pocket vetoes the bill after Congress has adjourned, the veto cannot be revoked.

local max is .5

step-by-step explanation:

the local maximum is for x values between 2 and 4

it looks like the x value is 2.5 and the y value is .5

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)