Puget Sound in the Magnolia neighborhood of Seattle, Washington. As the city’s largest public park, it contains 11.81 miles (19.01 km) of walking trails. The Discovery Park Loop Trail, designated a National Recreation Trail in 1975, runs 2.8 miles (4.5 km) through the park, connecting to other trails. Forests, beaches, prairies, and bluffs dominate the landscape of the park. Daybreak Star Cultural Center is within the park’s boundaries. The West Point Lighthouse is located on West Point, the westernmost point of the park and the entire city of Seattle. On the south side of the North Beach strip is the West Point Treatment Plant which is almost entirely concealed from the marsh, beach, and trail.- Magnolia, Seattle (Wikipedia)
Magnolia is the second largest neighborhood of Seattle, Washington by area. It occupies a hilly peninsula northwest of downtown. Magnolia has been a part of the city since 1891. A good portion of the peninsula is taken up by Discovery Park, formerly the U.S. Army’s Fort Lawton.
- Shilshole Bay (Wikipedia)
Shilshole Bay is the part of Puget Sound east of a line drawn northeasterly from Seattle’s West Point in the southwest to its Golden Gardens Park in the northeast. On its shores lie Discovery Park, the Lawton Wood section of the Magnolia neighborhood, the neighborhood of Ballard, and Golden Gardens Park. It is home to the Shilshole Bay Marina on Ballard’s Seaview Avenue N.W. and communicates with the Lake Washington Ship Canal via the Ballard Locks.
- 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.
- Permian (Wikipedia)
The Permian (/ˈpɜːrmi.ən/ PUR-mee-ən) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period 298.9 million years ago (Mya), to the beginning of the Triassic Period 251.902 Mya. It is the last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era. The concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the region of Perm in Russia.