I live in New York City. One of my favorite features about the city is Central Park- a cornucopia of fantastic schist boulders. There are so many awesome boulders in the park that there are legitimate places to free solo climb (its called Rat Rock! see linked video). I love how these boulders naturally outcrop and terraform the landscape and feel of the park. Anyone whose walked about on a beautiful day has likely been charmed by the paths naturally winding around fantastic rocks that pop up out of nowhere. Often, they are perfectly sloped and accessible enough to invite tourists to casually ascend for a better view. It's easy to find yourself sitting atop a massive boulder and wonder "how am I in the middle of a gigantic city right now??" The bedrock in the New York City region is mostly schist, a semi-hard metamorphic rock with loads of tiny crystals, mica flecks, and various bands of marble, quartz, and other fun stuff. The unique undulating slopes of Central Parks topology are all directly related to how this layer of schist has been adapting tectonically for billions of years. If you observe the exposed layers of rock, its immediately apparent its been through some heavy, dramatic movement. Look at the pictures and you'll see what I mean! I've included some various pics of Central Park from online. They aren't the best, but I work close by and will snap some real photos of my favorite spots!