Old Rocks
Diamond Member
#1 is an angular unconformity in sedimentary rock. Unconformities in Geology: Definition & Types - Video & Lesson Transcript | Study.comParroting outrageous time periods proves nothing.Crap, learn some geology in your kindergarden. LOLAll of which begin with general assumptions that the earth is 4 billion years old and everything has always been static. "Dumb fuck". Good one. Learn that in kindergarten last week?Look dumb fuck, there are many, many different methods of dating, and most scientists use several when trying to establish a date.I already answered your question yesterday- you lied about my answer and went on.
What you are doing is desperately dodging the question of why there is no evidence of modern man from 66 million years ago- even though you admit that the fish existed 66 million years ago.
Sure you did.
Why do you believe them when they say 66 million years?
The half-life of C14 is 5,730 years.
If you know how much C14 atoms were present at the time, you can calculate time.
Scientists assume the ratio of C14 is a constant.
C14 is formed in the atmosphere from cosmic rays.
I challenge it is not a constant ratio.
Geochronology - Wikipedia
Contents
[1Dating methods
If you were not so willfully ignorant, you would have looked them up before making an utter fool of yourself.
Precambrian Time
The Precambrian's lower limit is not defined, but ended about 542 million years ago. The Precambrian encompasses about 90% of Earth's history.
Eonothem eon Duration1 Eras Events
Archaean (Greek archaios = ancient ) 2,500? Eoarchean (Greek eos = dawn + archaios = ancient)
Paleoarchean (Greek palaios = old)
Mesoarchean (Greek mesos = middle)
Neoarchean (Greek neo = new) Formation of oceans,
atmosphere, and continents;
bacteria
Proterozoic (Greek proteros = earlier + zoön = animal) c. 2,000 Paleoproterozoic (Greek palaios = old)
Mesoproterozoic (Greek mesos = middle)
Neoproterozoic (Greek neo = new) Oxygen build-up;
multicelled organisms
1. In millions of years.
Paleozoic Era
This era began 542 million years ago and lasted about 291 million years. The name was compounded from Greek palaios (old) and zoön (animal).
Period Duration1 Epochs Events
Cambrian (Cambria, Latin name for Wales) 54 Lower Cambrian
Middle Cambrian
Upper Cambrian Invertebrate sea life proliferating during this and the following period
Ordovician (Latin Ordovices, people of early Britain) 45 Lower Ordovician
Upper Ordovician Diverse marine life, including vertebrates; vascular plants
Silurian (Latin Silures, people of early Wales) 28 Lower Silurian
Upper Silurian Coral reefs; giant scorpions; first jawed fish
Devonian (Devonshire in England) 57 Lower Devonian
Upper Devonian Numerous fishes, other sea life; many plants, first trees; wingless insects
Carboniferous (Latin carbo = coal + fero = to bear) 60 Upper, Middle, and
Lower Mississippian2
Upper, Middle, and
Lower Pennsylvanian2 Maximum coal formation in swampy forests; insects, amphibians, reptiles; fishes, clams, crustaceans
Permian (district of Perm in Russia) 48 Lower Permian
Upper Permian Large reptiles, amphibians; most species become extinct
1. In millions of years.
2. Mississippian and Pennsylvanian names are used only in the U.S.
Mesozoic Era
This era began 251 million years ago and lasted about 186 million years. The name was compounded from Greek mesos (middle) and zoön (animal). Popular name: Age of Reptiles.
Period Duration1 Epochs Events
Triassic (trias = triad) 51 Lower Triassic
Middle Triassic
Upper Triassic Early dinosaurs, crocodiles, turtles; first mammals
Jurassic (Jura Mountains) 54 Lower Jurassic
Middle Jurassic
Upper Jurassic Many seagoing reptiles; early large dinosaurs; later, flying reptiles (pterosaurs), earliest known birds
Cretaceous (Latin creta = chalk) 80 Lower Cretaceous
Upper Cretaceous Dinosaurs and other reptiles dominate; seed-bearing plants appear
1. In millions of years.
Cenozoic Era1
This era began 66 million years ago and includes the geological present. The name was compounded from Greek kainos (new) and zoön (animal). Popular name: Age of Mammals.
Period Duration2 Epochs Events
Paleogene (Greek palaios = old + genes = born) 42 Paleocene (Greek palaios = old + kainos = new). Eocene (Greek eos = dawn). Oligocene (Greek oligos = few). Rich insect fauna, early bats, increasingly diverse varieties of mammals and birds
Neogene (Greek neo = new + genes = born) 23 Miocene (Greek meios = less + kainos = new). Pliocene (Greek pleios = more). Pleistocene (Greek pleistos = most) (popular name: Ice Age). Holocene (Greek holos = entire), the last 10,000 years to the present. Further development of mammals and birds. Various forms of humans, including Homo sapiens
1. This table reflects the divisions used by the International Commission on Stratigraphy. The U.S. Geological Survey divides the Cenezoic Era into the Tertiary Period (with the Paleocene, Eocene, Oligocene, Miocene, and Pliocene Epochs) and the Quaternary Period (with the Pleistocene and Holocene Epochs).
2. In millions of years.
http://www.infoplease.com/ipa/A0001822.html
Now does that look static, you silly ass?
The geological layering suggests that a short, abrupt time period, not a long drawn out time period. You don't get the clean abrupt lines in a slow process that you see over the entire world.
View attachment 116846
Something else is missing in all these abrupt transition zones. There is no evidence of streams or rivers. At some point you should find where a river or stream once flowed.
But you do see geological layering with abrupt zones in rapid formations. Like this one in Mount St Helens.
View attachment 116847
You also do not need long periods of time to form features that "take millions of years of erosion". This one took a few months to form.
View attachment 116848
#2 appears to be a varved lake deposite
varved deposit | geology | Britannica.com
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Varved deposits attributed to sedimentation in Glacial Lake Missoula, Montana, U.S.
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#3 we have only your statement that coulee was created in a few months, no link. Looks like soft soils, so such is possible.