The document summarizes the geological time scale which divides Earth's history into different eras, periods, and epochs based on fossil and stratigraphic evidence. It describes the four eons of Earth's history starting with the Hadean and Archean eons of the earliest lifeforms like bacteria. It then outlines the major eras - Paleozoic, Mesozoic, and Cenozoic - describing some of the significant lifeforms, events, and environmental changes that occurred during each period within these eras. The largest unit of the geological time scale is the eon, while the smallest is the epoch.
The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronology (scientific branch of geology that aims to determine the age of rocks). It is used primarily by Earth scientists (including geologists, paleontologists, geophysicists, geochemists, and paleoclimatologists) to describe the timing and relationships of events in geologic history. The time scale has been developed through the study of rock layers and the observation of their relationships and identifying features such as lithologies, paleomagnetic properties, and fossils. The definition of standardized international units of geologic time is the responsibility of the International Commission on Stratigraphy (ICS), a constituent body of the International Union of Geological Sciences (IUGS), whose primary objective[1] is to precisely define global chronostratigraphic units of the International Chronostratigraphic Chart (ICC)[2] that are used to define divisions of geologic time. The chronostratigraphic divisions are in turn used to define geochronologic units.[2]
The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronology (scientific branch of geology that aims to determine the age of rocks). It is used primarily by Earth scientists (including geologists, paleontologists, geophysicists, geochemists, and paleoclimatologists) to describe the timing and relationships of events in geologic history. The time scale has been developed through the study of rock layers and the observation of their relationships and identifying features such as lithologies, paleomagnetic properties, and fossils. The definition of standardized international units of geologic time is the responsibility of the International Commission on Stratigraphy (ICS), a constituent body of the International Union of Geological Sciences (IUGS), whose primary objective[1] is to precisely define global chronostratigraphic units of the International Chronostratigraphic Chart (ICC)[2] that are used to define divisions of geologic time. The chronostratigraphic divisions are in turn used to define geochronologic units.[2]
While some regional terms are still in use,[3] the table of geologic time presented in this article conforms to the nomenclature, ages, and color codes set forth by the ICS as this is the standard, reference global geologic time scale – the International Geological Time Scale.[1][
The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronology (scientific branch of geology that aims to determine the age of rocks). It is used primarily by Earth scientists (including geologists, paleontologists, geophysicists, geochemists, and paleoclimatologists) to describe the timing and relationships of events in geologic history. The time scale has been developed through the study of rock layers and the observation of their relationships and identifying features such as lithologies, paleomagnetic properties, and fossils. The definition of standardized international units of geologic time is the responsibility of the International Commission on Stratigraphy (ICS), a constituent body of the International Union of Geological Sciences (IUGS), whose primary objective[1] is to precisely define global chronostratigraphic units of the International Chronostratigraphic Chart (ICC)[2] that are used to define divisions of geologic time. The chronostratigraphic divisions are in turn used to define geochronologic units.[2]
The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronology (scientific branch of geology that aims to determine the age of rocks). It is used primarily by Earth scientists (including geologists, paleontologists, geophysicists, geochemists, and paleoclimatologists) to describe the timing and relationships of events in geologic history. The time scale has been developed through the study of rock layers and the observation of their relationships and identifying features such as lithologies, paleomagnetic properties, and fossils. The definition of standardized international units of geologic time is the responsibility of the International Commission on Stratigraphy (ICS), a constituent body of the International Union of Geological Sciences (IUGS), whose primary objective[1] is to precisely define global chronostratigraphic units of the International Chronostratigraphic Chart (ICC)[2] that are used to define divisions of geologic time. The chronostratigraphic divisions are in turn used to define geochronologic units.[2]
While some regional terms are still in use,[3] the table of geologic time presented in this article conforms to the nomenclature, ages, and color codes set forth by the ICS as this is the standard, reference global geologic time scale – the International Geological Time Scale.[1][
Develop technical competence in basic principles of soil mechanics and fundamentals of application in engineering practice. (Outcomes b, e, k)
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Develop technical competence in basic principles of soil mechanics and fundamentals of application in engineering practice. (Outcomes b, e, k)
Ability to list the salient engineering properties of soils and their characteristics and describe the factors which control these properties. (Outcomes c)
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June 3, 2024 Anti-Semitism Letter Sent to MIT President Kornbluth and MIT Cor...Levi Shapiro
Letter from the Congress of the United States regarding Anti-Semitism sent June 3rd to MIT President Sally Kornbluth, MIT Corp Chair, Mark Gorenberg
Dear Dr. Kornbluth and Mr. Gorenberg,
The US House of Representatives is deeply concerned by ongoing and pervasive acts of antisemitic
harassment and intimidation at the Massachusetts Institute of Technology (MIT). Failing to act decisively to ensure a safe learning environment for all students would be a grave dereliction of your responsibilities as President of MIT and Chair of the MIT Corporation.
This Congress will not stand idly by and allow an environment hostile to Jewish students to persist. The House believes that your institution is in violation of Title VI of the Civil Rights Act, and the inability or
unwillingness to rectify this violation through action requires accountability.
Postsecondary education is a unique opportunity for students to learn and have their ideas and beliefs challenged. However, universities receiving hundreds of millions of federal funds annually have denied
students that opportunity and have been hijacked to become venues for the promotion of terrorism, antisemitic harassment and intimidation, unlawful encampments, and in some cases, assaults and riots.
The House of Representatives will not countenance the use of federal funds to indoctrinate students into hateful, antisemitic, anti-American supporters of terrorism. Investigations into campus antisemitism by the Committee on Education and the Workforce and the Committee on Ways and Means have been expanded into a Congress-wide probe across all relevant jurisdictions to address this national crisis. The undersigned Committees will conduct oversight into the use of federal funds at MIT and its learning environment under authorities granted to each Committee.
• The Committee on Education and the Workforce has been investigating your institution since December 7, 2023. The Committee has broad jurisdiction over postsecondary education, including its compliance with Title VI of the Civil Rights Act, campus safety concerns over disruptions to the learning environment, and the awarding of federal student aid under the Higher Education Act.
• The Committee on Oversight and Accountability is investigating the sources of funding and other support flowing to groups espousing pro-Hamas propaganda and engaged in antisemitic harassment and intimidation of students. The Committee on Oversight and Accountability is the principal oversight committee of the US House of Representatives and has broad authority to investigate “any matter” at “any time” under House Rule X.
• The Committee on Ways and Means has been investigating several universities since November 15, 2023, when the Committee held a hearing entitled From Ivory Towers to Dark Corners: Investigating the Nexus Between Antisemitism, Tax-Exempt Universities, and Terror Financing. The Committee followed the hearing with letters to those institutions on January 10, 202
2. What is the Earth’s time scale?
• The Geological time scale is a record of the life
forms and geological events in Earth’s history.
• Geologic time scale provides a system of
chronologic measurement relating Stratigraphy to
time that is used by geologist, paleontologist and
other earth scientists.
• Used to describe the timing and relationship b/w
events that have occurred during the history of
earth.
3. • Scientists developed the time scale by studying
rock layers and fossils world wide.
• Radioactive dating helped determine the
absolute divisions in the time scale.
• Geologist qualify the units as early, middle and
late when referring to time, and lower, mid and
upper when referring to the corresponding rocks.
4. Division of Geologic Time Scale
• Earth history is subdivided into time units based on:
– The fossil record
– Extinctions
5. Four Eons
• Pre-Archean or Hadean (4.6 to 3.8 Billion years)
~4.6 BYA -- Formation of Earth and Moon
~4 BYA -- Likely origin of life
• Archean (3.8 to 2.5 Billion years)
The eon of first life
~3.8 BYA -- Oldest known rocks
~3.5 BYA -- Oldest known fossils (single celled organisms resembling bacteria)
3.2 BYA -- First known plants (algae)
• Proterozoic (2.5 Billion to 570 Million years)
The eon of the first multicelled life
1.2 BYA -- First known animal (jellyfish)
• Phanerozoic (570 Million years to the Present)
• The eon of complex life
6. Divisions of Geologic Time
• Geological time begins with Precambrian
Time. Precambrian time covers approximately
88% of Earth’s history.
7. FOUR Eras…
• PRE-CAMBRIAN – 88% of earth’s history
• Paleozoic (ancient life)
– 544 million years ago…lasted 300 million yrs
• Mesozoic (middle life)
– 245 million years ago…lasted 180 million yrs
• Cenozoic (recent life)
– 65 million years ago…continues through present day
8. Today…
• Today we are in the Holocene Epoch of the
Quaternary Period of the Cenozoic Era.
Which unit is the largest?
Which unit is the smallest?
9.
10.
11. Paleozoic Era (Ancient Life)
• 542MYA ------- 250MYA
• The Paleozoic Era is broken up into six periods.
• The Cambrian period is the 1st period of the Paleozoic Era. “Age of the
Trilobites”.
• Ordovician Period: The only life on Earth was found in the seas.
However, by the end of the Ordovician Period, life moved to land.
Plants began to colonize out of the water paving the way in later
periods for animals to follow.
• The Silurian Period saw various invertebrates move on to land.
• The following period, the Devonian Period, saw vertebrates join the
other types of animals on land. The first ones to leave the water were
similar to amphibians and they eventually evolved into reptiles
12. Paleozoic Era
• The Carboniferous Period, is sometimes broken into
two separate periods called the Mississippian Period
and the Pennsylvanian Period.
• It is named the Carboniferous Period because much
of the coal we use today was made during the later
stages of this time period.
• The final period of the Paleozoic Era is the Permian
Period, the largest mass extinction ever on Earth
happened. This mass extinction, known as the
Permian Extinction, completely wiped out about 95%
of all life in the oceans on Earth.
13. Trilobites
• Lived in Earth’s ancient seas
• Extinct before the dinosaurs came
into existence
• Cambrian Period is know as the
“Age of the Trilobites” (put in on
table)
18. Mesozoic Era – Middle Life
• The Mesozoic Era is sometimes called "age of the dinosaurs“
• Began 250MYA.
• The Triassic Period: First small dinosaurs appeared in this
period.
• On land, the amphibians and small reptiles like turtles were
dominant during the early Triassic Period.
• The Jurassic Period: Larger and more abundant dinosaurs
appeared in this period.
• Land animals during the Jurassic Period had more diversity
• At the end of the Jurassic Period, birds evolved from
dinosaurs.
19. Mesozoic Era
• The Cretaceous Period:
• Flowering plants appeared during the END of
this era.
• On land, the first small mammals started to
appear during the Cretaceous Period
– The mammals were small, warm-blooded animals.
Hair covering their bodies.
20. Mesozoic Era
• The main plant life of this time were Gymnosperms
or plants that produce seeds, but no flowers.
• This era ended with a mass extinction event about 65
million years ago.
– Many groups of animals, including the dinosaurs
disappeared suddenly at this time.
• Many scientists believe that this event was caused by
a comet or asteroid colliding with the Earth.
22. Cenozoic Era – Recent Life
• Began about 65 million years ago and continues
today!!!!!
– Climate was warm and mild.
– Marine animals such as whales and dolphins evolved.
• Tertiary period:
– Paleogene
– Neogene
• Quaternary Period
• Mammals began to increase and evolve adaptations that
allowed them to live in many different environments –
land, air and the sea.
– Grasses increased and provided a food source for animals
23. Cenozoic Era
• Growth of mountains may have helped to cool down
the climate
– Ice Ages occurred late in the Cenozoic Era (Quaternary
Period).
• As the climate changed, the animals had to adapt to
the rise and fall of the oceans caused by melting
glaciers.
• This era is sometimes called the “Age of Mammals”
24. Cenozoic Era
• Marine animal examples:
– Algae, Mollusks, Fish and Mammals
• Land animal examples:
– Bats, Cats, Dogs, Cattle and Humans
– Humans are thought to have appeared around 3.5 million
years ago (during the most recent period – Quaternary).
• Flowering plants were now the most common plant
life.