[106871] in SIPB IPv6
I cannot believe this thing costs a fraction of a TV
daemon@ATHENA.MIT.EDU (Portable Projector)
Tue Aug 20 08:14:05 2019
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Date: Tue, 20 Aug 2019 08:13:50 -0400
From: "Portable Projector" <PortableProjector@projjecternano.pro>
Reply-To: "Portable Projector" <NanoHD@projjecternano.pro>
To: <sipbv6-mtg@charon2.mit.edu>
Message-ID: <q0oygr91pw2hcyql-pgo13bhjuavnat0q-241a-4356@projjecternano.pro>
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I cannot believe this thing costs a fraction of a TV
http://projjecternano.pro/nA6jY-7CjSifSgfYCoSnafqLmKK04XuwuNe9U21KATtl8w
http://projjecternano.pro/QNz68TXCIUQN4vzsClhkCJUHcHB74UJ8A3OUlH1jka5DMg
oks, canals and rivers, within an area of 3,842 square miles (9,951 km2), combine to form 38 main tributaries feeding the Thames between its source and Teddington Lock. This is the usual tidal limit; however, high spring tides can raise the head water level in the reach above Teddington and can occasionally reverse the river flow for a short time. In these circumstances, tidal effects can be observed upstream to the next lock beside Molesey weir, which is visible from the towpath and bridge beside Hampton Court Palace. Before Teddington Lock was built in 1810–12, the river was tidal at peak spring tides as far as Staines upon Thames.
In descending order, non-related tributaries of the non-tidal Thames, with river status, are the Churn, Leach, Cole, Ray, Coln, Windrush, Evenlode, Cherwell, Ock, Thame, Pang, Kennet, Loddon, Colne, Wey and Mole. In addition, there are occasional backwaters and artificial cuts that form islands, distributaries (most numerous in the case of the Colne), and man-made distributaries such as the Longford River. Three canals intersect this stretch: the Oxford Canal, Kennet and Avon Canal and Wey Navigation.
Its longest artificial secondary channel (cut), the Jubilee River, was built between Maidenhead and Windsor for flood relief and completed in 2002.
The non-tidal section of the river is owned and managed by the Environment Agency, which is responsible for managing the flow of water to help prevent and mitigate flooding, and providing for navigation: the volume and speed of water downstream is managed by adjusting the sluices at each of the weirs and, at peak high water, levels are generally dissipated over preferred flood plains adjacent to the river. Occasionally, flooding of inhabited areas is unavoidable and the agency issues flood warnings. Due to stiff penalties applicable on the non-tidal river, which is a drinking water source before treatment, sanitary sewer overflow from the many sewage treatment plants covering the upper Thames basin is rare in the non-tidal Thames, which ensures clearer water compared to the river's tidew
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<title>Newsletter</title>
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<span style="color:#FFFFFF;font-size:10px;">oks, canals and rivers, within an area of 3,842 square miles (9,951 km2), combine to form 38 main tributaries feeding the Thames between its source and Teddington Lock. This is the usual tidal limit; however, high spring tides can raise the head water level in the reach above Teddington and can occasionally reverse the river flow for a short time. In these circumstances, tidal effects can be observed upstream to the next lock beside Molesey weir, which is visible from the towpath and bridge beside Hampton Court Palace. Before Teddington Lock was built in 1810–12, the river was tidal at peak spring tides as far as Staines upon Thames. In descending order, non-related tributaries of the non-tidal Thames, with river status, are the Churn, Leach, Cole, Ray, Coln, Windrush, Evenlode, Cherwell, Ock, Thame, Pang, Kennet, Loddon, Colne, Wey and Mole. In addition, there are occasional backwaters and artificial cuts that form islands, distributaries (most numerous in the case of the Colne), and man-made distributaries such as the Longford River. Three canals intersect this stretch: the Oxford Canal, Kennet and Avon Canal and Wey Navigation. Its longest artificial secondary channel (cut), the Jubilee River, was built between Maidenhead and Windsor for flood relief and completed in 2002. The non-tidal section of the river is owned and managed by the Environment Agency, which is responsible for managing the flow of water to help prevent and mitigate flooding, and providing for navigation: the volume and speed of water downstream is managed by adjusting the sluices at each of the weirs and, at peak high water, levels are generally dissipated over preferred flood plains adjacent to the river. Occasionally, flooding of inhabited areas is unavoidable and the agency issues flood warnings. Due to stiff penalties applicable on the non-tidal river, which is a drinking water source before treatment, sanitary sewer overflow from the many sewage treatment plants covering the upper Thames basin is rare in the non-tidal Thames, which ensures clearer water compared to the river's tidew</span><br />
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