Mud, sand, and volcanic ash deposited in an early ocean.
Sediments buried and transformed into rock.
Formation of Ellsworth Schist, a metamorphic rock, the oldest on Mount Desert Island.
Collision of the micro-continent Avalonia with North America.
Formation of Bar Harbor Formation (layered sandstone and siltstone).
Volcanic activity created Cranberry Island Volcanics and ash layers.
Formation of Cadillac Mountain Granite, largest granite body on the island.
Shatter zones created where overlying rocks fell into molten granite.
Medium-grained granite formed west of Cadillac Mountain.
Later, diabase dikes intruded into granites and surrounding rocks.
Granite bodies exposed at the surface.
Softer surrounding rock eroded, leaving resistant granite mountains and ridges.
Streams and early ecosystems formed in valleys.
Northern North America repeatedly covered by ice sheets.
Each glaciation eroded earlier features, leaving traces of the most recent.
Ice sheets reached southern Maine.
Glaciers carved U-shaped valleys, polished mountains, and left striations and crescentic gouges.
Glaciers receded, leaving glacial erratics and deposits of rock, sand, and gravel.
Melting ice caused sea invasion in coastal Maine; formation of islands, beaches, and sea caves.
Lakes formed in valleys dammed by glacial debris (e.g., Jordan Pond).
Land rebounded; plants, animals, and humans colonized the area by ~9,000 years ago.
Ongoing erosion shapes granite ridges, cliffs, and rubble fields.
Coastal processes create beaches, cobble shores, and salt marshes.
Landscape continues to evolve due to water, wind, waves, and human impact.
Collision of the micro-continent
Example of striations caused by glacial movement