Looks like "что это", "what's this" in Russian. It may be seen when a Russian server player has the US keyboard and does not have the same characters. This is the most likely result.
A Russian dude: 4to 3to
A US dude: wot?
The Russian dude: Aw frick, I forgot to switch my keyboard lol
Also the Russian dude 1 minute later: что это
The US dude: Communist detected on American soil. Lethal force engaged.
A US dude: wot?
The Russian dude: Aw frick, I forgot to switch my keyboard lol
Also the Russian dude 1 minute later: что это
The US dude: Communist detected on American soil. Lethal force engaged.
by thealtf4psychic July 19, 2021
Conway's Game Of Life. NOT A GAME. This is a cellular automaton (CA) that has an infinite square grid of cells and uses the Moore neighbourhood along with the rule B3/S23 to determine the next generation.
Cells are either alive or dead.
A dead cell becomes alive if they have 3 alive neighbours. Alive cells stay alive if they have 2 or 3 alive neighbours. Otherwise, they either die or stay dead.
Cells are either alive or dead.
A dead cell becomes alive if they have 3 alive neighbours. Alive cells stay alive if they have 2 or 3 alive neighbours. Otherwise, they either die or stay dead.
by thealtf4psychic October 17, 2022
Paleontology is the study of geological events before (sometimes including) the Holocene Epoch which we currently live in. It includes the study of ancient organisms, extinction events, and changes to the Earth.
by thealtf4psychic April 22, 2021
The penultimate prime number before 100. A glitch prime of size 2. A Pythagorean prime (can be expressed as 4k+1). A Chen prime (89+2 is either a prime or a semiprime).
by thealtf4psychic September 02, 2022
The ultimate level of boredom. Typing the top-left corner checkerboard then the non-top-left corner checkerboard.
qetuosfhkzcbm and wryipadgjlxvn.
qetuosfhkzcbm and wryipadgjlxvn.
Someone whos fed up with playing chess: lemme search qetuosfhkzcbmwryipadgjlxvn lol WAIT URBDIC DOESN'T HAVE THIS WORD?!
by thealtf4psychic June 28, 2021
Rodinia is a relatively famous supercontinent that existed towards the end of the Proterozoic Eon. Nevertheless, many people don't know it. It existed from the Stenian period to right before the Cryogenian period encompassing nearly all of the Tonian period.
It was almost exactly on the opposite side of where Pangea formed. It turned inside out during the Cryogenian period to become Pannotia, leaving out exposed rocks that sucked up carbon dioxide, thus causing a snowball earth. Pannotia somehow still didn't make it into the Phanerozoic Eon.
Rodinia wasn't by itself unlike other supercontinents. It had a continent to the west of it as its companion. Made of parts of South America and Africa, this continent was called Congo. While Rodinia turned itself inside out, Congo got caught in between the two halves, completing Pannotia.
It was almost exactly on the opposite side of where Pangea formed. It turned inside out during the Cryogenian period to become Pannotia, leaving out exposed rocks that sucked up carbon dioxide, thus causing a snowball earth. Pannotia somehow still didn't make it into the Phanerozoic Eon.
Rodinia wasn't by itself unlike other supercontinents. It had a continent to the west of it as its companion. Made of parts of South America and Africa, this continent was called Congo. While Rodinia turned itself inside out, Congo got caught in between the two halves, completing Pannotia.
Jack who lives in eastern South America: Bruh, my point 800 million years ago was in Congo and not in the rest of Rodinia. Why were the bacteria that lived where I am not able to party with everyone else until 720 million years ago? I feel bad for them.
Kate who lives in western Africa: The bacteria that lived where I am partied with the bacteria that lived where you are for billions of years! Don't feel bad when it comes to paleogeography or paleontology. There are always good things behind terrible extinction events and isolation from everyone else.
Kate who lives in western Africa: The bacteria that lived where I am partied with the bacteria that lived where you are for billions of years! Don't feel bad when it comes to paleogeography or paleontology. There are always good things behind terrible extinction events and isolation from everyone else.
by thealtf4psychic April 20, 2021
Comprising of the Paleoproterozoic, Mesoproterozoic and Neoproterozoic Eras, This eon spans from 2.5 billion years ago to 541 million years ago lasting almost 2 billion years.
During the beginning of this eon, cyanobacteria rapidly reproduced and photosynthesized turning a lot of carbon dioxide to oxygen. This oxygen reacted with the iron in the oceans, filling the oceans with iron rust BIFs, turning the oceans blood red. Later, there was no longer enough iron to hold onto the oxygen, and it escaped into the atmosphere. That oxygen formed the ozone layer. Nearly all of the carbon dioxide turned into oxygen, turning earth into a snowball earth.
The snowball earth quickly recovered after 300 million years. Then, supercontinent Columbia formed. For the next billion years, climate remained notably stable. This period of time from 1.8 billion years to 800 million years ago was called "The boring billion". During this period, supercontinent Rodinia formed, but broke apart. The rocks that became exposed sucked up more carbon dioxide from volcanoes, turning earth into a second snowball earth.
After that recovered, the two halves of Rodinia reunited around the South Pole forming supercontinent Pannotia. However, it broke apart during the end of the eon just as animals started to appear, as Laurentia rifted away from the rest of the supercontinent. Finally, the End-Ediacaran extinction event took place to end the eon.
During the beginning of this eon, cyanobacteria rapidly reproduced and photosynthesized turning a lot of carbon dioxide to oxygen. This oxygen reacted with the iron in the oceans, filling the oceans with iron rust BIFs, turning the oceans blood red. Later, there was no longer enough iron to hold onto the oxygen, and it escaped into the atmosphere. That oxygen formed the ozone layer. Nearly all of the carbon dioxide turned into oxygen, turning earth into a snowball earth.
The snowball earth quickly recovered after 300 million years. Then, supercontinent Columbia formed. For the next billion years, climate remained notably stable. This period of time from 1.8 billion years to 800 million years ago was called "The boring billion". During this period, supercontinent Rodinia formed, but broke apart. The rocks that became exposed sucked up more carbon dioxide from volcanoes, turning earth into a second snowball earth.
After that recovered, the two halves of Rodinia reunited around the South Pole forming supercontinent Pannotia. However, it broke apart during the end of the eon just as animals started to appear, as Laurentia rifted away from the rest of the supercontinent. Finally, the End-Ediacaran extinction event took place to end the eon.
Imagine living during the middle of the Proterozoic Eon! There would be no plants, no animals, just water, land and bacteria!
by thealtf4psychic March 30, 2021