Gay City State playground is recognized for the lakeside shores, but the park reveals a substantial amount of Connecticut geology besides
- Igneous
- Pegmatite
Gay city-state Park is acknowledged for the lakeside beaches, however, the park discloses an important level of Connecticut geology aswell
- Metamorphic
- Amphibolite
- Schist
- Gneiss
Gay City State Park is acknowledged for the lakeside beaches, but the playground shows a significant quantity of Connecticut geology at the same time
- Sedimentary
- Nothing
Gay city-state playground is acknowledged for their lakeside beaches, however, the playground shows an important app gratis rate my date quantity of Connecticut geology nicely
- Collins mountain Formation (Ordovician): Metavolcanic representative comprising schist, gneiss, and amphibolite
When you go into the park from course 85, follow the park road and bear to the left where in actuality the highway forks. After the trail is actually a little parking area with an entrance to your white trail resulting in the Mill Site.
The very first huge structure from the white trail try a classic factory website, located on the remaining area (Figure 1 and 4). The foundation from the mill can nevertheless be viewed, and the chute that leads with the tiny stream that streams by. The building blocks from the factory try predominantly constructed from gneiss, a high-grade metamorphic rock put through intensive temperature and pressure during formation. Gneiss is readily identifiable from the segregation of light and black vitamins providing they a banded surface.
During the factory website, the flow on your own right has a higher metal concentration within the water (Figure 2). Because of this highest iron attention, water provides a red tinge.