I am trying to understand the geodesic flow on the following 2-dimensional Riemannian manifold $M$. As a set, $M$ is the interior of the standard 2-simplex,
$$M=\{(x,y)\in\mathbb{R}^2\mid x,y>0~\text{and}~x+y<1\}.$$
The metric on $M$ is given by
$$ds^2=\left(\frac{1}{x}+\frac{1}{1-x-y}\right)\,dx^2+2\left(\frac{1}{1-x-y}\right)\,dxdy+\left(\frac{1}{y}+\frac{1}{1-x-y}\right)\,dy^2.$$
A direct calculation shows that $M$'s Gaussian curvature is given by the positive constant $K=\frac{1}{4}$. Therefore, the Killing-Hopf theorem tells us that $M$ is not geodesically complete; if it were, Killing-Hopf, together with the simple observation that $M$ is simply connected, would imply that $M$ is isometric to the sphere, which is not true.
My question has two parts:
(1) Is the dimension of $M$'s isometry group greater than zero? Note that, even though $M$ is locally isometric to the sphere, with its 3-dimensional isometry group, $M$'s isometry group must have fewer dimensions than 3. If the dimension was $3$, $M$ would be a homogeneous space, and would therefore be geodesically complete (impossible for the reason stated above).
(2) Can you find an example of a geodesic that is not defined on all of $\mathbb{R}$? I'm having trouble visualizing "why" $M$ is not-geodesically complete. Is the problem that certain geodesics can run off the simplex in finite time, or is it something else?