In ye _really_ olden days people used to read email on a box connected to a large server somewhere, using a textbased piece of software like elm (for electronic mail) or pine (because geeks like puns).
A bit later, people needed to be able to download email from a server onto their own machines so they could read them there, and free up some more space in their online mailbox. To do this they used the Post Office Protocol (or POP) to connect, download all new emails and then disconnect again. The problem with this was that once you'd downloaded them onto your computer they couldn't easily be on any other computer. Which meant that you ended up either forwarding them to your other accounts (or yourself) to read later, or just doing without.
And then came IMAP. the Internet Message Access Protocol. This allowed you to leave the messages on the server, which would keep them _forever_ - and your email client would connect to it and just tell you what messages were sitting there. If you marked a message as read (or replied to) then that marking would happen _on the server_ and you would see exactly the same view no matter what computer you were on.
However, some geeks had been using the internet for a very long time, or had been told once that POP was how you downloaded email, and they never tried out IMAP, despite it being much more useful. Especially now that you can have gigabytes of email sitting online without worrying about space restraints.
But nowadays even GMail supports it. And it's dead handy. So give it a go.
(This post prompted by
johanna_alice, who wass having problems reading email on two machines, and was doing all sorts of complex things to work around it, when IMAP would have solved the problems instantly.)
A bit later, people needed to be able to download email from a server onto their own machines so they could read them there, and free up some more space in their online mailbox. To do this they used the Post Office Protocol (or POP) to connect, download all new emails and then disconnect again. The problem with this was that once you'd downloaded them onto your computer they couldn't easily be on any other computer. Which meant that you ended up either forwarding them to your other accounts (or yourself) to read later, or just doing without.
And then came IMAP. the Internet Message Access Protocol. This allowed you to leave the messages on the server, which would keep them _forever_ - and your email client would connect to it and just tell you what messages were sitting there. If you marked a message as read (or replied to) then that marking would happen _on the server_ and you would see exactly the same view no matter what computer you were on.
However, some geeks had been using the internet for a very long time, or had been told once that POP was how you downloaded email, and they never tried out IMAP, despite it being much more useful. Especially now that you can have gigabytes of email sitting online without worrying about space restraints.
But nowadays even GMail supports it. And it's dead handy. So give it a go.
(This post prompted by
no subject
Date: 2008-03-10 09:54 pm (UTC)no subject
Date: 2008-03-10 09:56 pm (UTC)Personally I find it terribly distracting a lot of the time. I prefer the thunderbird interface.
Other people prefer the Outlook interface.
Or a variety of other programs.
It means that we can read our email in any program we like, rather than being stuck with the one we're given.
no subject
Date: 2008-03-10 10:00 pm (UTC)no subject
Date: 2008-03-10 10:06 pm (UTC)And POP doesn't support the notion of folders at all.
You can't do this with POP:
no subject
Date: 2008-03-10 10:48 pm (UTC)POP3 lets you do the following:
That's it - the sum total. You can set your mail client to never delete anything from your maildrop, but there's no way to organise your mail on the server side.
IMAP allows you to do the following:
POP3 gives you a PO box. IMAP gives you a filing cabinet.
no subject
Date: 2008-03-10 11:02 pm (UTC)no subject
Date: 2008-03-11 08:19 am (UTC)no subject
Date: 2008-03-11 09:57 am (UTC)no subject
Date: 2008-03-10 09:54 pm (UTC)no subject
Date: 2008-03-10 09:57 pm (UTC)no subject
Date: 2008-03-10 10:34 pm (UTC)no subject
Date: 2008-03-10 10:46 pm (UTC)no subject
Date: 2008-03-10 11:37 pm (UTC)no subject
Date: 2008-03-10 09:59 pm (UTC)old skool
Date: 2008-03-10 10:02 pm (UTC)no subject
Date: 2008-03-10 10:28 pm (UTC)no subject
Date: 2008-03-10 10:41 pm (UTC)no subject
Date: 2008-03-10 10:58 pm (UTC)no subject
Date: 2008-03-11 08:28 am (UTC)Don't know about searching. But I do know that it's Mac's preferred method:
http://www.apple.com/dotmac/mail.html
no subject
Date: 2008-03-11 12:27 am (UTC)no subject
Date: 2008-03-11 03:58 pm (UTC)no subject
Date: 2008-03-11 03:59 pm (UTC)no subject
Date: 2008-03-11 09:33 am (UTC)By the way, do you happen to know if IMAP handles duplicate messages efficiently (that is, does it store n copies of each message sent to a mailing list with n recipients on the server, or just one shared copy)? The reason I ask is that (a) the university mail servers are chronically short of space and (b) we get a LOT of talk announcements and other spam-like things, and I suspect that (a) is partly due to (b).
no subject
Date: 2008-03-11 09:45 am (UTC)no subject
Date: 2008-03-11 03:57 pm (UTC)I set up gmail to archive the emails that I download onto my computer. So they're all still there and searchable, but they aren't filling up my inbox.
no subject
Date: 2008-03-11 06:16 pm (UTC)no subject
Date: 2008-03-12 09:02 am (UTC)no subject
Date: 2008-03-11 07:47 pm (UTC)no subject
Date: 2008-03-12 08:49 am (UTC)And because I can get to my email from my phone, I have all of my flight information (for instance) available for me wherever I am.
Bits of paper get lost. And the last bit of post that was actually worth keeping was my mortgage documents - 9 months ago.