Every day, the citizens of the Internet send each other billions of e-mail messages. If you're online a lot, you yourself may send a dozen or more e-mails each day without even thinking about it. Obviously, e-mail has become an extremely popular communication tool.
Have you ever wondered how e-mail gets from your computer to a friend halfway around the world? What is a POP3 server, and how does it hold your mail? The answers may surprise you, because it turns out that e-mail is an incredibly simple system at its core. In this article, we'll take an in-depth look at e-mail and how it works.
According to Darwin Magazine: Prime Movers, the first e-mail message was sent in 1971 by an engineer named Ray Tomlinson. Prior to this, you could only send messages to users on a single machine. Tomlinson's breakthrough was the ability to send messages to other machines on the Internet, using the @ sign to designate the receiving machine.
An e-mail message has always been nothing more than a simple text message -- a piece of text sent to a recipient. In the beginning and even today, e-mail messages tend to be short pieces of text, although the ability to add attachments now makes many messages quite long. Even with attachments, however, e-mail messages continue to be text messages.
You've probably already received several e-mail messages today. To look at them, you use some sort of e-mail client. Many people use well-known, stand-alone clients like Microsoft Outlook, Outlook Express, Eudora or Pegasus. People who subscribe to free e-mail services like Hotmail or Yahoo use an e-mail client that appears in a Web page. If you're an AOL customer, you use AOL's e-mail reader. No matter which type of client you're using, it generally does four things:
Sophisticated e-mail clients may have all sorts of bells and whistles, but at the core, this is all that an e-mail client does.
Given that you have an e-mail client on your machine, you are ready to send and receive e-mail. All that you need is an e-mail server for the client to connect to. Let's imagine what the simplest possible e-mail server would look like in order to get a basic understanding of the process. Then we will look at the real thing.
If you've read How Web Servers Work, then you know that machines on the Internet can run software applications that act as servers. There are Web servers, FTP servers, telnet servers and e-mail servers running on millions of machines on the Internet right now. These applications run all the time on the server machine and they listen to specific ports, waiting for people or programs to attach to the port. The simplest possible e-mail server would work something like this:
From: jsmith To: mbrain Marshall, Can we have lunch Monday? John
There are several other pieces of information that the server might save into the file, like the time and date of receipt and a subject line; but overall, you can see that this is an extremely simple process.
We'll look at the SMTP server in the next section.
As other people sent mail to mbrain, the server would simply append those messages to the bottom of the file in the order that they arrived. The text file would accumulate a series of five or 10 messages, and eventually I would log in to read them. When I wanted to look at my e-mail, my e-mail client would connect to the server machine. In the simplest possible system, it would:
When I double-clicked on a message header, it would find that message in the text file and show me its body.
As you can see, this is a very simple system. Surprisingly, the real e-mail system that you use every day isn't much more complicated than this.
For the vast majority of people right now, the real e-mail system consists of two different servers running on a server machine. One is called the SMTP server, where SMTP stands for Simple Mail Transfer Protocol. The SMTP server handles outgoing mail. The other is either a POP3 server or an IMAP server, both of which handle incoming mail. POP stands for Post Office Protocol, and IMAP stands for Internet Mail Access Protocol. A typical e-mail server looks like this:
The SMTP server listens on well-known port number 25, POP3 listens on port 110 and IMAP uses port 143 (see How Web Servers Work for details on ports).
Whenever you send a piece of e-mail, your e-mail client interacts with the SMTP server to handle the sending. The SMTP server on your host may have conversations with other SMTP servers to deliver the e-mail.
Let's assume that I want to send a piece of e-mail. My e-mail ID is brain, and I have my account on howstuffworks.com. I want to send e-mail to This email address is being protected from spambots. You need JavaScript enabled to view it.. I am using a stand-alone e-mail client like Outlook Express.
When I set up my account at howstuffworks, I told Outlook Express the name of the mail server -- mail.howstuffworks.com. When I compose a message and press the Send button, here's what happens:
If, for some reason, the SMTP server at HowStuffWorks cannot connect with the SMTP server at Mindspring, then the message goes into a queue. The SMTP server on most machines uses a program called sendmail to do the actual sending, so this queue is called the sendmail queue. Sendmail will periodically try to resend the messages in its queue. For example, it might retry every 15 minutes. After four hours, it will usually send you a piece of mail that tells you there is some sort of problem. After five days, most sendmail configurations give up and return the mail to you undelivered.
The SMTP server understands very simple text commands like HELO, MAIL, RCPT and DATA. The most common commands are:
In the simplest implementations of POP3, the server really does maintain a collection of text files -- one for each e-mail account. When a message arrives, the POP3 server simply appends it to the bottom of the recipient's file.
When you check your e-mail, your e-mail client connects to the POP3 server using port 110. The POP3 server requires an account name and a password. Once you've logged in, the POP3 server opens your text file and allows you to access it. Like the SMTP server, the POP3 server understands a very simple set of text commands. Here are the most common commands:
USER - enter your user ID
PASS - enter your password
QUIT - quit the POP3 server
LIST - list the messages and their size
RETR - retrieve a message, pass it a message number
DELE - delete a message, pass it a message number
TOP - show the top x lines of a message, pass it a message number and the number of lines
Your e-mail client connects to the POP3 server and issues a series of commands to bring copies of your e-mail messages to your local machine. Generally, it will then delete the messages from the server (unless you've told the e-mail client not to).
You can see that the POP3 server simply acts as an interface between the e-mail client and the text file containing your messages. And again, you can see that the POP3 server is extremely simple. You can connect to it through telnet at port 110 and issue the commands yourself if you would like to (see How Web Servers Work for details on telnetting to servers).
The IMAP Server
As you can see, the POP3 protocol is very simple. It allows you to have a collection of messages stored in a text file on the server. Your e-mail client (e.g. Outlook Express) can connect to your POP3 e-mail server and download the messages from the POP3 text file onto your PC. That is about all that you can do with POP3.
Many users want to do far more than that with their e-mail, and they want their e-mail to remain on the server. The main reason for keeping your e-mail on the server is to allow users to connect from a variety of machines. With POP3, once you download your e-mail it's stuck on the machine to which you downloaded it. If you want to read your e-mail both on your desktop machine and your laptop (depending on whether you're working in the office or on the road), POP3 makes life difficult.
IMAP (Internet Mail Access Protocol) is a more advanced protocol that solves these problems. With IMAP, your mail stays on the e-mail server. You can organize your mail into folders, and all the folders live on the server as well. When you search your e-mail, the search occurs on the server machine, rather than on your machine. This approach makes it extremely easy for you to access your e-mail from any machine, and regardless of which machine you use, you have access to all of your mail in all of your folders.
We'll look at IMAP problems and attachments in the next section.
Your e-mail client connects to the IMAP server using port 143. The e-mail client then issues a set of text commands that allow it to do things like list all the folders on the server, list all the message headers in a folder, get a specific e-mail message from the server, delete messages on the server or search through all of the e-mails on the server.
One problem that can arise with IMAP involves this simple question: "If all of my e-mail is stored on the server, then how can I read my mail if I'm not connected to the Internet?" To solve this problem, most e-mail clients have some way to cache e-mail on their local machine. For example, the client will download all the messages and store their complete contents on the local machine (just like it would if it were talking to a POP3 server). The messages still exist on the IMAP server, but you now have copies on your machine. This allows you to read and reply to e-mail even if you have no connection to the Internet. The next time you establish a connection, you download all the new messages you received while disconnected and send all the mail that you wrote while disconnected.
Your e-mail client allows you to add attachments to e-mail messages you send, and also lets you save attachments from messages that you receive. Attachments might include word processing documents, spreadsheets, sound files, snapshots and pieces of software. Usually, an attachment is not text (if it were, you would simply include it in the body of the message). Since e-mail messages can contain only text information, and attachments aren't text, there's a problem that needs to be solved.
In the early days of e-mail, you solved this problem by hand, using a program called uuencode. The uuencode program assumes that the file contains binary information. It extracts 3 bytes from the binary file and converts them to four text characters (that is, it takes 6 bits at a time, adds 32 to the value of the 6 bits and creates a text character -- see How Bits and Bytes Work to learn more about ASCII characters). What uuencode produces, therefore, is an encoded version of the original binary file that contains only text characters. In the early days of e-mail, you would run uuencode yourself and paste the uuencoded file into your e-mail message.
Considering its tremendous impact on society, having forever changed the way we communicate, today's e-mail system is one of the simplest things ever devised! There are parts of the system, like the routing rules in sendmail, that get complicated, but the basic system is incredibly straightforward. The next time you send an e-mail, you'll know exactly how it's getting to its destination.
Check out the next page for simple etiquette rules about writing and sending e-mail messages.
Whether it's for work or keeping in touch with family and friends, people rely on the Internet to send and receive e-mail messages. According to a March 2007 study by the Pew Internet and American Life Project, 91 percent of U.S. Internet users have gone online to send or read e-mail. The same source reports that 56 percent of e-mail users send or read e-mail as part of a typical day [source: Email Marketing Reports].
An October 2007 study by the market research firm, The Radicati Group, reported that 183 billion e-mails were sent daily in 2006. With numbers like that, it's no surprise that there's a large variety of e-mail service providers to choose from. Choices include providers like Gmail or Yahoo! who provide free e-mail service or providers who charge a fee like America Online, Apple or NetZero.
Gmail and Yahoo! make money from advertisers who pay them to expose e-mail account holders to their messages. It's also easy to find reviews of various free e-mail services. Here are few descriptions of free e-mail services:
E-mail providers who charge a fee may offer additional services such as increased storage space. Sample providers include Juno, EarthLink and Webmail.us.
For example, it's easier to get personalized e-mail addresses -- perhaps incorporating your actual name, for instance - using a paid service. Paid e-mail services often allow users to keep their same e-mail address even if they change their ISP and screen users from advertisers. They often are easier to reach on support issues and special features such as custom spam filters, additional e-mail accounts and mobile access.
Most ISP Internet providers can also serve as an e-mail provider for no additional charge. Other paid e-mail services specialize in small business accounts and can assist businesses in purchasing and maintaining a domain name.
On the next page, we'll offer some etiquette tips for when you write and send e-mail messages.
Most people wouldn't think of being rude or obnoxious when they speak to colleagues, clients or their supervisor. But those rules can fall by the wayside when we use e-mail.
The opportunities for rudeness when using e-mail are plentiful and not always easy to recognize. Most people wouldn't use foul language or derogatory terms in business communication. But what about raising one's voice? Is that possible when using e-mail?
Here, we'll discuss some business writing rules and tips for practicing e-mail etiquette.
People are busy, so:
People are sensitive, so:
Not everyone is as hip as you are, so:
E-mail is like as a business letter. Ignoring basic rules can show disrespect for the recipient. Don't let informality spoil the recipient's opinion of you.
For lots more information about e-mail and related topics, check out the links on the next page.