From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #17052 Reply-To: ammf@fruvous.com Sender: owner-ammf-digest@smoe.org Errors-To: owner-ammf-digest@smoe.org Precedence: bulk alt.music.moxy-fruvous digest Thursday, December 11 2025 Volume 14 : Number 17052 Today's Subjects: ----------------- "Sleep Like Royalty â Luxurious Sheets for the New Season" ["Miracle Affi] ---------------------------------------------------------------------- Date: Thu, 11 Dec 2025 01:52:56 -0600 From: "Miracle Affiliate Team" Subject: "Sleep Like Royalty â Luxurious Sheets for the New Season" "Sleep Like Royalty b Luxurious Sheets for the New Season" http://nukelyt.space/tp6n3Sd82VAu_KeSV-aSrmpfnEyTU40FOJl-hnLQ4eDxOsrQbw http://nukelyt.space/ENF9hRG3ni9msPBQmrr0Uw59-7dZwa4b2z_0hOh0I_A0I7Ev3A ers are categorized by their morphology, thermal characteristics, and behavior. Alpine glaciers form on the crests and slopes of mountains. A glacier that fills a valley is called a valley glacier, or alternatively, an alpine glacier or mountain glacier. A large body of glacial ice astride a mountain, mountain range, or volcano is termed an ice cap or ice field. Ice caps have an area less than 50,000 km2 (19,000 sq mi) by definition. Glacial bodies larger than 50,000 km2 (19,000 sq mi) are called ice sheets or continental glaciers. Several kilometers deep, they obscure the underlying topography. Only nunataks protrude from their surfaces. The only extant ice sheets are the two that cover most of Antarctica and Greenland. They contain vast quantities of freshwater, enough that if both melted, global sea levels would rise by over 70 m (230 ft). Portions of an ice sheet or cap that extend into water are called ice shelves; they tend to be thin with limited slopes and reduced velocities. Narrow, fast-moving sections of an ice sheet are called ice streams. In Antarctica, many ice streams drain into large ice shelves. Some drain directly into the sea, often with an ice tongue, like Mertz Glacier. Tidewater glaciers are glaciers that terminate in the sea, including most glaciers flowing from Greenland, Antarctica, Baffin, Devon, and Ellesmere Islands in Canada, Southeast Alaska, and the Northern and Southern Patagonian Ice Fields. As the ice reaches the sea, pieces break off or calve, forming icebergs. Most tidewater glaciers calve above sea level, which often results in a tremendous impact as the iceberg strikes the water. Tidewater glaciers undergo centuries-long cycles of advance and retreat that are much less affected by climate cha ------------------------------ End of alt.music.moxy-fruvous digest V14 #17052 ***********************************************