I Think I’m Gonna Rebrand…..

Bear without fur……musty ahh….

Looks llike a Chupacabra

But just more disappointing

Ski… bi… di….

Standing eggs

🗣️🗣️🔥🔥🔥🔥 those were the days

listening to hits from the 1400 BC guys

Aquarius Cookie is here! ♒️ I held a poll on insta and had my followers vote on which zodiac cookie they’d wanna see next. I knew I wanted to give him a surfer dude/beachy vibe since Aquarius is such a confident, outgoing sign. Also water gun > vase to fit the beach theme (also lowkey inspired by kobo kanaeru lmao)

Listen to this

OH GGOD. OH FINALLY FUCKING GOD. I'M FREE. FREE. I AM. FREE

FREE YOU HEAR

EXAMS WERE HELL, AND WILL REMAIN HELL BUT AT LEAST I NOT STRESSED.

I literally just had my oral. And like. I was the first and I finished so fucking quickly. But hey atleast I can read the passage. Ughdhdhfnfnf

I'm free finally oh good god you have blessed me. Ahhhhhhhhhhbhh

Haaahahahahahahahahahahahaba

HEHEHEHEHEHEEHEHHE

I'M BACK BABEYYYYYY

HAGGGSGSHSHDHDBSNAJSJ

ARRRGHHHHH

IM CRYING. I DON'T KNOW IF IT'S TEARS OF JOY OR STRESS BUT I AM CRYONG

Elden here I come 😈😈

And also it's time to speed run my asks 👹👹

An extremely late introduction to myself.

Hellos. I won’t say that I’m exactly new to Tumblr but I’ve hidden myself amongst the canopy of other active Tumblr posters. However on the behest of my most beloved spouse (in the most platonic way ever) I have decided to reveal myself.

Hi, you guys can call me Theo and I am a *minor*. So to those 18 and above you’d have to shoo away. I’d say that I have plenty of interest such as:

Elden Ring (Current hyper fixation)

Genshin Impact

Honkai: Star Rail

Honkai Impact 3rd

Project Sekai (Maybe vocaloids in general…)

Dungeons & Dragons (!!!)

Madoka Magica

IHNMAIMS (kinda)

EPIC: The Musical

I think that’s it.

Other than interests, I also have hobbies. (Of course) My only hobby is art, and to be more specific drawing. I have dabbled in sculpting and painting a couple of times but not as often as I would drawing. I am more of a traditional artist than a digital one (Having started drawing with a pencil since I can grab one.) I have started on digital around the start of 2023 and has tried to practice ever since.

I would say that I would be a more art based Tumblr blog. But that wouldn’t mean I would post often… I feel like this would turn into a place where I would ramble on and on about my of lore (and a place to store it too).

This concludes my introduction. Thank you for taking your time to read this and I hope that you have fun around here :):)

The spouse, the skrunkle! @the-redacted-of-all-time (they cool bros)

Literally left you guys for a damn camp.

Anyways, it’s raining as all heck here. I promise that I will continue working on that animatic broskis

New favourite art genre: lucas cranach germany 1500s ill matched couples

me and my pooks @the-redacted-of-all-time (I’m the stinky old man)

The oldest material found in the Solar System is dated to 4.5682+0.0002

−0.0004 Ga (billion years) ago.[35] By 4.54±0.04 Ga the primordial Earth had formed.[36] The bodies in the Solar System formed and evolved with the Sun. In theory, a solar nebula partitions a volume out of a molecular cloud by gravitational collapse, which begins to spin and flatten into a circumstellar disk, and then the planets grow out of that disk with the Sun. A nebula contains gas, ice grains, and dust (including primordial nuclides). According to nebular theory, planetesimals formed by accretion, with the primordial Earth being estimated as likely taking anywhere from 70 to 100 million years to form.[37]

Estimates of the age of the Moon range from 4.5 Ga to significantly younger.[38] A leading hypothesis is that it was formed by accretion from material loosed from Earth after a Mars-sized object with about 10% of Earth's mass, named Theia, collided with Earth.[39] It hit Earth with a glancing blow and some of its mass merged with Earth.[40][41] Between approximately 4.1 and 3.8 Ga, numerous asteroid impacts during the Late Heavy Bombardment caused significant changes to the greater surface environment of the Moon and, by inference, to that of Earth.[42]

Earth's atmosphere and oceans were formed by volcanic activity and outgassing.[43] Water vapor from these sources condensed into the oceans, augmented by water and ice from asteroids, protoplanets, and comets.[44] Sufficient water to fill the oceans may have been on Earth since it formed.[45] In this model, atmospheric greenhouse gases kept the oceans from freezing when the newly forming Sun had only 70% of its current luminosity.[46] By 3.5 Ga, Earth's magnetic field was established, which helped prevent the atmosphere from being stripped away by the solar wind.[47]

As the molten outer layer of Earth cooled it formed the first solid crust, which is thought to have been mafic in composition. The first continental crust, which was more felsic in composition, formed by the partial melting of this mafic crust.[49] The presence of grains of the mineral zircon of Hadean age in Eoarchean sedimentary rocks suggests that at least some felsic crust existed as early as 4.4 Ga, only 140 Ma after Earth's formation.[50] There are two main models of how this initial small volume of continental crust evolved to reach its current abundance:[51] (1) a relatively steady growth up to the present day,[52] which is supported by the radiometric dating of continental crust globally and (2) an initial rapid growth in the volume of continental crust during the Archean, forming the bulk of the continental crust that now exists,[53][54] which is supported by isotopic evidence from hafnium in zircons and neodymium in sedimentary rocks. The two models and the data that support them can be reconciled by large-scale recycling of the continental crust, particularly during the early stages of Earth's history.[55]

New continental crust forms as a result of plate tectonics, a process ultimately driven by the continuous loss of heat from Earth's interior. Over the period of hundreds of millions of years, tectonic forces have caused areas of continental crust to group together to form supercontinents that have subsequently broken apart. At approximately 750 Ma, one of the earliest known supercontinents, Rodinia, began to break apart. The continents later recombined to form Pannotia at 600–540 Ma, then finally Pangaea, which also began to break apart at 180 Ma.[56]

The most recent pattern of ice ages began about 40 Ma,[57] and then intensified during the Pleistocene about 3 Ma.[58] High- and middle-latitude regions have since undergone repeated cycles of glaciation and thaw, repeating about every 21,000, 41,000 and 100,000 years.[59] The Last Glacial Period, colloquially called the "last ice age", covered large parts of the continents, to the middle latitudes, in ice and ended about 11,700 years ago.[60]

Chemical reactions led to the first self-replicating molecules about four billion years ago. A half billion years later, the last common ancestor of all current life arose.[61] The evolution of photosynthesis allowed the Sun's energy to be harvested directly by life forms. The resultant molecular oxygen (O2) accumulated in the atmosphere and due to interaction with ultraviolet solar radiation, formed a protective ozone layer (O3) in the upper atmosphere.[62] The incorporation of smaller cells within larger ones resulted in the development of complex cells called eukaryotes.[63] True multicellular organisms formed as cells within colonies became increasingly specialized. Aided by the absorption of harmful ultraviolet radiation by the ozone layer, life colonized Earth's surface.[64] Among the earliest fossil evidence for life is microbial mat fossils found in 3.48 billion-year-old sandstone in Western Australia,[65] biogenic graphite found in 3.7 billion-year-old metasedimentary rocks in Western Greenland,[66] and remains of biotic material found in 4.1 billion-year-old rocks in Western Australia.[67][68] The earliest direct evidence of life on Earth is contained in 3.45 billion-year-old Australian rocks showing fossils of microorganisms.[69][70]

During the Neoproterozoic, 1000 to 539 Ma, much of Earth might have been covered in ice. This hypothesis has been termed "Snowball Earth", and it is of particular interest because it preceded the Cambrian explosion, when multicellular life forms significantly increased in complexity.[72][73] Following the Cambrian explosion, 535 Ma, there have been at least five major mass extinctions and many minor ones.[74] Apart from the proposed current Holocene extinction event, the most recent was 66 Ma, when an asteroid impact triggered the extinction of non-avian dinosaurs and other large reptiles, but largely spared small animals such as insects, mammals, lizards and birds. Mammalian life has diversified over the past 66 Mys, and several million years ago, an African ape species gained the ability to stand upright.[75][76] This facilitated tool use and encouraged communication that provided the nutrition and stimulation needed for a larger brain, which led to the evolution of humans. The development of agriculture, and then civilization, led to humans having an influence on Earth and the nature and quantity of other life forms that continues to this day.[77]

YESSSS, FEED ME KNOWLEDGE

(Did you copy and paste from Wikipedia)

(And I’m also writing this in school😈)