What would the geology and climate of a supposed landmass near the pole be like, assuming a thoroughly warmer planet? I am designing a fantasy setting for pen-and-paper role-playing (and potential novel) purposes. I have decided that a continent be situated right on a Pole of some imaginary planet with axial tilt comparable to Earth. My question is: is it possible to achieve environmental conditions in the Continent at least somewhat similar to those of current-day Europe?

My understanding of Earth climate is that the poles, while extremely cold, are also very dry in terms of precipitation. I have understood that this is mostly due to the axial tilt but I'm not sure. I have heard that in a warmer part of Earth's history the poles had vegetation - is this possible even with the ever-present high-pressure zone?

I guess one way the continent could be habitable is to be full of freshwater rivers, originating from glaciers high atop of some mountains. I guess such mountains are plausible near the pole (I don't think the movement and mutual interaction of continental plates are somehow dependent of the latitude, are they?)

Thank's in advance for your great contributions!
For a very basic explanation of why poles are the way they are, note that the amount of solar radiation coming from the sun is spread over a larger area at the pole. Therefore you get less radiation per square meter. As a result it is colder.

Cold air can hold less water vapour. As such it is very dry (in terms of water mass per air volume) in cold regions. Dry air obviously can provide less precipitation. If your polar continent is warmer, you'll see more precipitation.

Large-scale weather phenomena are indeed mostly driven by Earth's rotation. As such you have somewhat more stable conditions along the poles. However, complex topography (i.e. mountains) can severely interfere with these conditions. This is the reason why the stratospheric ozone hole is much smaller in the northern hemisphere than in the southern hemisphere: There is much more mixing between differnt air regions in the north. In the troposphere this effect is even more pronounced.