From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #17008 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 Saturday, November 29 2025 Volume 14 : Number 17008 Today's Subjects: ----------------- How To Get Hard & Stay Hard Naturally ["James" ] Say Goodbye to Night Driving Struggles! ["Night Vision Pro Deal" ] Vintage-Inspired Ceramic Christmas Tree Night Light ["Warm Glow" Subject: How To Get Hard & Stay Hard Naturally How To Get Hard & Stay Hard Naturally http://wavmint.fun/8nofWwia8UGbTGocnP15ZUVzLSpp8z7fBBxDIAjJPKv6zbzqiQ http://wavmint.fun/Vsu5Y4CASy6yFNgpasBjFtZaAQOY9rzhcLC-UQMoUL9ehK_Uaw n horse breed best known for its colorful spotted coat pattern. There is a wide range of body types within the breed, stemming from the influence of multiple breeds of horses throughout its history. Each horse's color pattern is genetically the result of various spotting patterns overlaid on top of one of several recognized base coat colors. The color pattern of the Appaloosa is of interest to those who study equine coat color genetics, as it and several other physical characteristics are linked to the leopard complex mutation (LP). Appaloosas are prone to develop equine recurrent uveitis and congenital stationary night blindness; the latter has been linked to the leopard complex. Artwork depicting prehistoric horses with leopard spotting exists in prehistoric cave paintings in Europe. Images of domesticated horses with leopard spotting patterns appeared in artwork from Ancient Greece and Han dynasty China through the early modern period. In North America, the Nez Perce people of what today is the United States Pacific Northwest developed the original American spotted breed. Settlers once referred to these spotted horses as the "Palouse horse", possibly after the Palouse River, which ran through the heart of Nez Perce country. Gradually, the name evolved into Appaloosa. The Nez Perce lost most of their horses after the Nez Perce War in 1877, and the breed fell into decline for several decades. A small number of dedicated breeders preserved the Appaloosa as a distinct breed until the Appaloosa Horse Club (ApHC) was formed as the breed registry in 1938. The modern breed maintains bloodlines tracing to the foundation bloodstock of the registry; its partially open stud book allows the addition of some Thoroughbred, American Quarter Horse and Arabian blood. Today, the Appaloosa is one of the most popular breeds in the United States; it was named the state horse of Idaho in 1975. It is best known as a stock horse used in a num ------------------------------ Date: Sat, 29 Nov 2025 13:18:17 +0100 From: "Night Vision Pro Deal" Subject: Say Goodbye to Night Driving Struggles! Say Goodbye to Night Driving Struggles! http://truehatch.ru.com/n9NsSj_ki8q6nheINNGmtdMP9BHJXK_VZt9CLj_r0lpJylgdRA http://truehatch.ru.com/AQORTqGqIOzvd6xBLKQwLNN1Cjg_0k4SP-j8-cHdDA3j6nWdQw ck (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the crust, and most of its interior, except for the liquid outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathering, transport, and deposition of existing rocks. Metamorphic rocks are formed when existing rocks are subjected to such high pressures and temperatures that they are transformed without significant melting. Humanity has made use of rocks since the time the earliest humans lived. This early period, called the Stone Age, saw the development of many stone tools. Stone was then used as a major component in the construction of buildings and early infrastructure. Mining developed to extract rocks from the Earth and obtain the minerals within them, including metals. Modern technology has allowed the development of new human-made rocks and rock-like substances, s ------------------------------ Date: Sat, 29 Nov 2025 11:16:12 +0100 From: "InHeat" Subject: Absolutely perfect for the office Absolutely perfect for the office http://flowenhance.space/PvuZ_L1iEN2YgfgqqyXBRi3_s2qwhKcf4aTTRHgbNAQ8TaxLbg http://flowenhance.space/weW16bBN0DdURZougkzXphz0n9IhlIwq6QJqMxYEV34qZZaV1g il is a major component of the Earth's ecosystem. The world's ecosystems are impacted in far-reaching ways by the processes carried out in the soil, with effects ranging from ozone depletion and global warming to rainforest destruction and water pollution. With respect to Earth's carbon cycle, soil acts as an important carbon reservoir, and it is potentially one of the most reactive to human disturbance and climate change. As the planet warms, it has been predicted that soils will add carbon dioxide to the atmosphere due to increased biological activity at higher temperatures, a positive feedback (amplification). This prediction has, however, been questioned on consideration of more recent knowledge on soil carbon turnover. Soil acts as an engineering medium, a habitat for soil organisms, a recycling system for nutrients and organic wastes, a regulator of water quality, a modifier of atmospheric composition, and a medium for plant growth, making it a critically important provider of ecosystem services. Since soil has a tremendous range of available niches and habitats, it contains a prominent part of the Earth's genetic diversity. A gram of soil can contain billions of organisms, belonging to thousands of species, mostly microbial and largely still unexplored. Soil has a mean prokaryotic density of roughly 108 organisms per gram, whereas the ocean has no more than 107 prokaryotic organisms per milliliter (gram) of seawater. Organic carbon held in soil is eventually returned to the atmosphere through the process of respiration carried out by heterotrophic organisms, but a substantial part is retained in the soil in the form of soil organic matter; tillage usually increases the rate of soil respiration, leading to the depletion of soil organic matter. Since plant roots need oxygen, aeration is an important characteristic of soil. This ventilation can be accomplished via networks of interconnected soil pores, which also absorb and hold rainwater making it readily available for uptake by plants. Since plants require a nearly continuous supply of water, but most regions receive sporadic rainfall, the water-holding capacity of soils is vital for plant survival. Soils can effectively remove impurities, kill disease agents, and degrade contaminants, this latter property being called natural attenuation. Typically, soils maintain a net absorption of oxygen and methane and undergo a net release of carbon dioxide and nitrous oxide. Soils offer plants physical sup ------------------------------ Date: Sat, 29 Nov 2025 09:51:36 -0600 From: "Warm Glow" Subject: Vintage-Inspired Ceramic Christmas Tree Night Light Vintage-Inspired Ceramic Christmas Tree Night Light http://seroburn.ru.com/uu8mfSB6Sg2ezs9nNvyapIln76WkkLcDuOEsSE7OxeJ-VRW9ww http://seroburn.ru.com/aOC71E8416EsPcbuYW795_3SB84LM4qomSp67SOEA7lwhp36kA ed in agriculture, where it serves as the anchor and primary nutrient base for plants. The types of soil and available moisture determine the species of plants that can be cultivated. Agricultural soil science was the primeval domain of soil knowledge, long time before the advent of pedology in the 19th century. However, as demonstrated by aeroponics, aquaponics and hydroponics, soil material is not an absolute essential for agriculture, and soilless cropping systems have been claimed as the future of agriculture for an endless growing mankind. Soil material is also a critical component in mining, construction and landscape development (also called landscape architecture) industries. Soil serves as a foundation for most construction projects. The movement of massive volumes of soil can be involved in surface mining, road building and dam construction. Earth sheltering is the architectural practice of using soil for external thermal mass against building walls. Many building materials are soil based. Loss of soil through urbanization is growing at a high rate in many areas and can be critical for the maintenance of subsistence agriculture. Soil resources are critical to the environment, as well as to food and fibre production, producing 98.8% of food consumed by humans. Soil provides minerals and water to plants according to several processes involved in plant nutrition. Soil absorbs rainwater and releases it later, thus preventing floods and drought, flood regulation being one of the major ecosystem services provided by soil. Soil cleans water as it percolates through it. Soil is the main or the sole habitat for many soil organisms: the major part of known and unknown biodiversity is in the soil, in the form of earthworms, woodlice, millipedes, centipedes, snails, slugs, mites, springtails, enchytraeids, nematodes, protists), bacteria, archaea, fungi and algae; and most organisms living above ground have part of them (plants) or spend part of their life cycle (e.g. insects) below-ground. Above-ground and below-ground biodiversities are tightly interconnected, making soil protection of paramount importance for any restoration or conservation plan. The biological component of soil is an extremely important carbon sink since about 57% of the biotic content is carbon. Even in deserts, cyanobacteria, lichens and mosses form biological soil crusts which capture and sequester a significant amount of carbon by photosynthesis. Intensive farming and gra ------------------------------ Date: Sat, 29 Nov 2025 01:11:55 -0600 From: "Your Barista" Subject: Your reward is waiting Your reward is waiting http://selfsufficient.za.com/a4Vttj_ByK3lHX8DMN0HH3BT6xiBlhIqzb9nJN1ZYyrzDczW http://selfsufficient.za.com/yOJSiAU8QSpUXpZDcTBtucVZWbirwdxFJx892xIOaovqNTpuyQ ck (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the crust, and most of its interior, except for the liquid outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathering, transport, and deposition of existing rocks. Metamorphic rocks are formed when existing rocks are subjected to such high pressures and temperatures that they are transformed without significant melting. Humanity has made use of rocks since the time the earliest humans lived. This early period, called the Stone Age, saw the development of many stone tools. Stone was then used as a major component in the construction of buildings and early infrastructure. Mining developed to extract rocks from the Earth and obtain the minerals within them, including metals. Modern technology has allowed the development of new human-made rocks and rock-like substances, s ------------------------------ Date: Thu, 27 Nov 2025 14:45:30 -0800 From: "MES | Services Australia" Subject: Medicare Appointment Receipt for Friday, 28 November 2025 Medicare Australia b Appointment Confirmation Medicare Australia b Appointment Confirmation This is a reminder about your upcoming Medicare appointment. Date: Friday, 28 November 2025 Location: Nearest Service Center Access and Download your Appointment Confirmation Receipt Here https://tinyurl.com/zukww8zw You may be required to sign in to your online Medicare account to securely access the downloaded receipt and view the complete details of your appointment. This message was sent automatically by the Medicare appointment system. Please do not reply to this email. ------------------------------ End of alt.music.moxy-fruvous digest V14 #17008 ***********************************************