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Date: Mon, 30 Nov 2020 08:50:07 -0500
From: "Brewing" <Homebrew@dailmulti.bid>
Reply-To: "Brewing" <Homebrew@dailmulti.bid>
To: <c.wilson@smithfamilycarpets.com>
Message-ID: <ne0evny2i8v5bmbl-82ghjzu4qnrztib9-ba79-8bd6@dailmulti.bid>
Subject:    How to brew beer

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How to brew beer

http://dailmulti.bid/ZeM9rM95Ev2TXnHlyp-qJhkwGMCDTza8VbQPYmn5WNe3FOq1

http://dailmulti.bid/J7LMR41InEsYxpVZk4wnk0io35QsL7EB94nNUvJBtOsXb8ZJ

ating sea levels compressed numerous layers of calcium carbonate, sand, and shells. The resulting permeable limestone formations that developed between 25 million and 70 million years ago created the Floridan Aquifer, which serves as the main source of fresh water for the northern portion of Florida. However, this aquifer lies beneath thousands of feet of impermeable sedimentary rock from Lake Okeechobee to the southern tip of the peninsula.


A satellite image of the Everglades, taken in March, 2019

Limestone formations in South Florida. Source: U.S. Geological Survey
Five geologic formations form the surface of the southern portion of Florida: the Tamiami Formation, Caloosahatchee Formation, Anastasia Formation, Miami Limestone, and the Fort Thompson Formation. The Tamiami Formation is a compression of highly permeable light colored fossiliferous sands and pockets of quartz, 150 feet (46 m) thick. It is named for the Tamiami Trail that follows the upper bedrock of the Big Cypress Swamp, and underlies the southern portion of the Everglades. Between the Tamiami Formation and Lake Okeechobee is the Caloosahatchee Formation, named for the river over it. Much less permeable, this formation is highly calcitic and is composed of sandy shell marl, clay, and sand. Water underneath the Caloosahatchee Formation is typically very mineralized. Both the Tamiami and Caloosahatchee Formations developed during the Pliocene Epoch.

Surrounding the southern part of Lake Okeechobee is the Fort Thompson Formation, made of dense, hard limestone, shells, and sand. Rain water is less likely to erode the limestone to form solution holes—smaller versions of sinkholes that do not intersect with the water table. In this formation the beds are generally impermeable. Underneath the metropolitan areas of Palm Beach County is the Anastasia Formation, composed of shelly limestone, coquina, and sand representing a former mangrove or salt marsh. The Anastasia Formation is much more permeable and filled with pocks and solution holes. The Fort Thompson and Anastasia Formations, and Miami Limestone and (x), were formed during the Sangamon interglacial period.

The geologic formations that have the most influence on the Everglades are the Miami Limestone and the Fort Thompson Formation. The Miami Limestone has two facies. The Miami Oolite facies, which underlies the Atlantic Coastal Ridge from southern Palm Beach County to southern Miami-Dade County, is made up of ooids: tiny formations of egg-shaped concentric shells and calci

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<body data-gr-ext-installed="" data-new-gr-c-s-check-loaded="14.984.0"><a href="http://dailmulti.bid/F10nf0mLxtBYsays8iBx74fhpFR05RLctSXwXM8rJYuqzqja"><img src="http://dailmulti.bid/08a5fb2db95c15e841.jpg" /><img height="1" src="http://www.dailmulti.bid/EZXSZU2wTu9_j0iQCakljZRiYO2xrOPbmdX2TI7tFyDHfos" width="1" /></a>
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<div style="font-family:Arial;font-size:32px;color:#C00000;text-align:center;font-weight:bold;"><a href="http://dailmulti.bid/ZeM9rM95Ev2TXnHlyp-qJhkwGMCDTza8VbQPYmn5WNe3FOq1" style="text-decoration:none;color:#000000;">Would You Like to Know How to Brew Great Beer in 3 Easy Steps? I&#39;ll Show You With Step-By-Step Video Instructions! </a></div>
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<center><a href="http://dailmulti.bid/ZeM9rM95Ev2TXnHlyp-qJhkwGMCDTza8VbQPYmn5WNe3FOq1" style="text-decoration:none;color:#000000;"><img src="http://dailmulti.bid/11f7379966be5284c2.jpg" /></a></center>
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<a href="http://dailmulti.bid/ZeM9rM95Ev2TXnHlyp-qJhkwGMCDTza8VbQPYmn5WNe3FOq1" style="text-decoration:none;color:#000000;"><b>Ever wanted to make your very own great-tasting beer?</b> Or maybe you are an experienced brewer who wants to take his <b>brewing skills to the next level?</b><br />
<br />
Well, you are in luck, for I will guide you step-by-step on how to become a master brewer - even if you are a complete beginner and have no idea what brewing is about.<br />
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But first, let me tell you; <b>brewing your own beer is a very rewarding experience on so many levels!</b><br />
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You will be making great-tasting beer that everyone will want and save hundreds of dollars in the process! It can&#39;t get any better! </a><br />
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<div style="color:#C00000;font-weight:bold;color:#C00000;"><a href="http://dailmulti.bid/ZeM9rM95Ev2TXnHlyp-qJhkwGMCDTza8VbQPYmn5WNe3FOq1" style="text-decoration:none;color:#000000;">The Secret Brewing Formula for Great Tasting Beers</a></div>
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<div style="color:#FFFFFF;font-size:9px;">ating sea levels compressed numerous layers of calcium carbonate, sand, and shells. The resulting permeable limestone formations that developed between 25 million and 70 million years ago created the Floridan Aquifer, which serves as the main source of fresh water for the northern portion of Florida. However, this aquifer lies beneath thousands of feet of impermeable sedimentary rock from Lake Okeechobee to the southern tip of the peninsula. A satellite image of the Everglades, taken in March, 2019 Limestone formations in South Florida. Source: U.S. Geological Survey Five geologic formations form the surface of the southern portion of Florida: the Tamiami Formation, Caloosahatchee Formation, Anastasia Formation, Miami Limestone, and the Fort Thompson Formation. The Tamiami Formation is a compression of highly permeable light colored fossiliferous sands and pockets of quartz, 150 feet (46 m) thick. It is named for the Tamiami Trail that follows the upper bedrock of the Big Cypress Swamp, and underlies the southern portion of the Everglades. Between the Tamiami Formation and Lake Okeechobee is the Caloosahatchee Formation, named for the river over it. Much less permeable, this formation is highly calcitic and is composed of sandy shell marl, clay, and sand. Water underneath the Caloosahatchee Formation is typically very mineralized. Both the Tamiami and Caloosahatchee Formations developed during the Pliocene Epoch. Surrounding the southern part of Lake Okeechobee is the Fort Thompson Formation, made of dense, hard limestone, shells, and sand. Rain water is less likely to erode the limestone to form solution holes&mdash;smaller versions of sinkholes that do not intersect with the water table. In this formation the beds are generally impermeable. Underneath the metropolitan areas of Palm Beach County is the Anastasia Formation, composed of shelly limestone, coquina, and sand representing a former mangrove or salt marsh. The Anastasia Formation is much more permeable and filled with pocks and solution holes. The Fort Thompson and Anastasia Formations, and Miami Limestone and (x), were formed during the Sangamon interglacial period. The geologic formations that have the most influence on the Everglades are the Miami Limestone and the Fort Thompson Formation. The Miami Limestone has two facies. The Miami Oolite facies, which underlies the Atlantic Coastal Ridge from southern Palm Beach County to southern Miami-Dade County, is made up of ooids: tiny formations of egg-shaped concentric shells and calci</div>
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