[226484] in SIPB-AFS-requests
Don't Let Neuropathy Slow You Down - Grounded Footwear is Now Half Price!
daemon@ATHENA.MIT.EDU (Grounded Footwear)
Thu Feb 27 09:53:20 2025
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Date: Thu, 27 Feb 2025 15:53:18 +0100
From: "Grounded Footwear" <GroundedFootwear@cardiofend.sa.com>
Reply-To: "Grounded Footwear" <Grounded@cardiofend.sa.com>
Subject: Don't Let Neuropathy Slow You Down - Grounded Footwear is Now Half Price!
To: <sipb-afsreq-mtg@charon.mit.edu>
Message-ID: <zw5soux35atfhgga-zkljp5w3r5l1lw02-2c395-5176f@cardiofend.sa.com>
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Don't Let Neuropathy Slow You Down - Grounded Footwear is Now Half Price!
http://cardiofend.sa.com/IZ0YvLJuTQ0JWp_c51tk02hO8ezi_6vcGEJbfd2zh6FRwyyCBw
http://cardiofend.sa.com/KS__PrC4wIITPg72lFpyJLvIxOgEKlj72KHbwr8rP5tN9Mrcqw
se about 1000 square kilometers and rest in the southern Maya Mountains, whilst the lower basin is known as the Mountain Pine Ridge catchment. The soils in the upper watershed tend to be shallow and rocky, leading to rapid runoff. All of the upper catchment tributaries join the mainstem channel considerably before Guacamayo, the approximate join point of the two connecting sub-sheds of the Macal River. Peak flows follow the rainy season of June to August, with tailing rains until February; lowest flows are in the dry season from March to May.
For the lower Macal River catchment (or Mountain Pine Ridge area), tributary streams are arranged radially to feed the mainstem; principal lower basin rivers are the Privassion, Rio On, Rio Frio, Mollejon, Chaa Creek and Cacao Camp. In the lower catchment basin, there is considerable overland friction to surface runoff due to the dense terrestrial detrititus and understory on the forest floor, even though the forest canopy itself is sometimes sparse. The retarded runoff of this lower sub-watershed allows the rapid peak runoff of the upper watershed to overtake the flow within Mountain Pine Ridge, forming an effective single massive peak wave, which exacerbates downstream flooding in the Belize River, and, in fact, controls the flood stage of the larger Belize River. This effect of simultaneous peak flow is further enhanced by the radial geometry of the lower Macal Basin tributaries, encouraging all sub-basin flow to reach the mainstem at approximately the sa
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<div style="color:#FFFFFF;font-size:8px;">se about 1000 square kilometers and rest in the southern Maya Mountains, whilst the lower basin is known as the Mountain Pine Ridge catchment. The soils in the upper watershed tend to be shallow and rocky, leading to rapid runoff. All of the upper catchment tributaries join the mainstem channel considerably before Guacamayo, the approximate join point of the two connecting sub-sheds of the Macal River. Peak flows follow the rainy season of June to August, with tailing rains until February; lowest flows are in the dry season from March to May. For the lower Macal River catchment (or Mountain Pine Ridge area), tributary streams are arranged radially to feed the mainstem; principal lower basin rivers are the Privassion, Rio On, Rio Frio, Mollejon, Chaa Creek and Cacao Camp. In the lower catchment basin, there is considerable overland friction to surface runoff due to the dense terrestrial detrititus and understory on the forest floor, even though the forest canopy itself is sometimes sparse. The retarded runoff of this lower sub-watershed allows the rapid peak runoff of the upper watershed to overtake the flow within Mountain Pine Ridge, forming an effective single massive peak wave, which exacerbates downstream flooding in the Belize River, and, in fact, controls the flood stage of the larger Belize River. This effect of simultaneous peak flow is further enhanced by the radial geometry of the lower Macal Basin tributaries, encouraging all sub-basin flow to reach the mainstem at approximately the sa</div>
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