First, recall that once we start discussing lines in , the notion of “slope” needs to be revisited. A key observation is that lines with different “slopes” in the -plane actually point in different directions, so it is a natural idea to replace “slope” with a vector parallel to the line.
Now, note that the line exists independently of the parameterization that we use to describe it; different choices of the parameter will trace out the line in different fashions, but they trace out the same line.
Consider the line in given by .
- If we require that , then , and a parameterization of the line is
- If we require that , then , and a parameterization of the line is
Note that the line passes through the point . The vector-valued function will trace through this point at , while the vector-valued function will trace through this point at .
To find a vector parallel to the line , note that we can write the line in the form
A vector parallel to the line is thus .