Apashanka said:
For a geodesic curve in 2-D polar coordinates(r,θ) the tangent vector is ##V=\hat r##
There is an ambiguity in your statement. You talk about "a geodesic curve in 2-D polar coordinates". You haven't specified a connection, and I'm not sure if you are familiar with the concept of a connection. This is unfortunate, because the covariant derivative isn't uniquely specified unless one defines a connection.
Now, in GR, it is implied that when we talk about a "geodesic curve", we use the Levi-Civita connection. Often, we get lazy about stating this explicitly. If we assume that's what you meant, then there is a subset of geodesic curves in the plane, namely those geodesic curves that pass through the origin, that have a tangent vector of ##\hat{r}##.
However, there are also a large set of geodesic curves with the Levi-Civita connection that don't pass through the origin, and whose tangent vector is something different.
What I think is probably happening is that when you are talking about 'using 2-D polar coordinates', you really mean that you are using a connection other than the Levi-Civiti connection. But I could be wrong about what you're trying to say.
The most striking thing about your posts is that you seem to think that specifying the coordinates matters. It doesn't. Once we specify that we are using the Levi-Civiti connection on the plane, geodesic curves are always the curve of shortest distance between two points. This is hopefully familiar an intuitive.
Then the point is that he curve that is the shortest distance between two points on the plane exists, and is independent of the coordinates used. We don't need to talk about whether we are using polar coordinates or cartesian coordinates to talk about the curve that is the shortest distance between two points.
What I suspect is happening is that you are wandering into the realms of connections other than the Levi-Civita connection without realizing it. Circles about the origin, curves with a constant value for the r coordinate, are not geodesics in the Levi-Civita connection, but may be geodesics with some other connection. But when one opens up the possibility of using connections other than the Levi-Civita connection, one needs to realize that covariant derivatve operators are not unique.
I suspect that it's least confusing at this point to restrict oneself to the Levi-Civiti connection on the plane (or other flat manifolds), as a steppingstone to talking about geodesics with the Levi-Civita connection on manifolds that are not necessiarly flat, and then moving onto using connections that aren't the Levi-Civita connection. But this is not the only way to do things, it's just the way that I'd recommend.