- Bellingham, Washington
- Blakely Harbor
- Deception Pass
- Deception Pass (gravelbeach.blogspot.com)
Much of Puget Sound is nothing but Pleistocene - with Vashon glacial deposits on the surface and older glacial and interglacial sediments peaking out from the lower portions of some of the bluffs. But at Rocky Point, on the west side of Whidbey Island, and in Skagit Bay, the Mesozoic re-emerges from the basement to form rocky islands and headlands.
Deception Pass looking east- Elevators take visitors to an observation deck 520 ft (160 m) above ground in 41 seconds, which offers panoramic views of the downtown Seattle skyline, the Olympic and Cascade Mountains, Mount Rainier, Mount Baker, Elliott Bay, and various islands in Puget Sound.
- Everett, Washington
Ferry under the purple sky- Fidalgo Island
- Golden Gardens has exceptional views of Puget Sound and the Olympic Mountains across the sound.
- Hood Canal
- Hood Canal and the rest of Puget Sound were created about 13,000 years ago, during the Late Pleistocene, by the Puget Lobe of the Cordilleran Ice Sheet.
Looking northwest from Richmond Beach Saltwater Park
On the deck toward Vashon Island- Possession Sound
- Puget Sound (Wikipedia)
Puget Sound (/ˈpjuːdʒɪt/ PEW-jit) is a sound of the Pacific Northwest, an inlet of the Pacific Ocean, and part of the Salish Sea. It is located along the northwestern coast of the U.S. state of Washington. It is a complex estuarine system of interconnected marine waterways and basins, with one major and two minor connections to the open Pacific Ocean via the Strait of Juan de Fuca—Admiralty Inlet being the major connection and Deception Pass and Swinomish Channel being the minor.
- Puget Sound lies to the west of the town, including an unincorporated area known as Point Wells.
Railroad to the Tacoma Narrows Bridge- Salish Sea
- Seattle
- Skagit River
- Stillaguamish River
- Tacoma Narrows Bridge
- Tacoma, Washington
- The name “Broadview” was given to the neighborhood because of its panoramic views of the Puget Sound and Olympic Mountains, which can be viewed to the west from its steep, westerly hillsides.
- The Vashon Glaciation is an extension of the Fraser Glaciation in which the Cordilleran Ice Sheet advanced south of the present day Canada–United States border into the Puget Sound region.
- Titlow Park
- Vashon glacier begins to melt and recede from Puget Sound region and Columbia Basin around 16,900 years ago (historylink.org)
- Washington
- Blue Ridge, Seattle
- Broadview, Seattle
- Burien, Washington
- Des Moines, Washington
- Everett, Washington
- Magnolia, Seattle
- Meadowdale, Washington
- Mukilteo, Washington
- Normandy Park, Washington
- Olympia, Washington
- Olympic Peninsula
- Picnic Point, Washington
- Seattle
- Sunset Hill, Seattle
- Tacoma, Washington
- Washington
- incomplete list
