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The Mattachine Steps, also known as the Cove Avenue stairway, is an outdoor staircase in Silver Lake, Los Angeles, in the U.S. state of California, dedicated to the Mattachine Society in 2012 in memory of Harry Hay, who cofounded the gay rights group.
The name "Drukken" steps derives from a person's gait as they stepped from stone to stone whilst crossing the Red Burn. Seven or more stones were originally set in the Red Burn which was much wider than in 2009. [3] Burns himself used the Scots spelling "Drucken" rather than "Drukken". [4] The ruins of the Drukken Steps are in the Eglinton ...
Watershed delineation is the process of identifying the boundary of a watershed, also referred to as a catchment, drainage basin, or river basin.It is an important step in many areas of environmental science, engineering, and management, for example to study flooding, aquatic habitat, or water pollution.
This list is from the Database of British and Irish Hills ("DoBIH") in October 2018, and are peaks the DoBIH marks as being Wainwrights ("W"). [b] [13] DoBIH also updates the measurements as surveys are recorded, so these tables should not be amended unless the entire DoBIH data is re-downloaded; these measurements may differ slightly from the "By Book" section, which are from older sources.
Stairs are a structure designed to bridge a large vertical distance between lower and higher levels by dividing it into smaller vertical distances. This is achieved as a diagonal series of horizontal platforms called steps which enable passage to the other level by stepping from one to another step in turn.
The lake is part of the Grand Rounds National Scenic Byway, connecting with Lake of the Isles on the northeast, Cedar Lake and Brownie Lake on the northwest, and Lake Harriet on the south. The Minneapolis Park and Recreation Board trail system has a 3.4-mile (5.5 km) trail around the lake for bicyclists and skaters and a 3.2-mile (5.1 km) trail ...
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Lake stratification is the tendency of lakes to form separate and distinct thermal layers during warm weather. Typically stratified lakes show three distinct layers: the epilimnion, comprising the top warm layer; the thermocline (or metalimnion), the middle layer, whose depth may change throughout the day; and the colder hypolimnion, extending to the floor of the lake.
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