SlideShare a Scribd company logo
1 of 22
Tidal Theory
By: Jackelyn Diaz
BSEd-Bio. Sci.II
Tidal theory-- a theory of the evolution of a
celestial body that is based on the action of tidal
forces; specify
: such a theory explaining the moon's
evolution.
It is the application of continuum mechanics to
interpret and predict the tidal deformations of
planetary and satellite bodies and their atmospheres
and oceans, under the gravitational loading of another
astronomical body or bodies. It commonly refers to
the fluid dynamic motions for the Earth's oceans.
Tides—motion caused by the
gravitational attraction
between the earth, moon and
sun.
Newton (Theory of Gravity)—
tides are caused by a differential
gravitational pull.
Spring tides—sun, moon and earth
are all aligned. The tides are high. It
occurs twice a month during full
moon and new moon.
♥The gravitational pull of the moon
and sun are combined. At these
times, the high tides are very high
and the low tides are very low.
Neap tides—moon and sun
are at right angles to each
other. Tidal extremes are
reduced. It occurs during 1st
and 3rd quarter of the moon.
Absolute
and
Relative
Dating
Relative Dating—It is the science
determining the relative order of past
events, without necessarily
determining their absolute age.
♦It is when you know the age of a
certain rock layer is by comparing the
fossils.
♦It can only determine the sequential
order in which a series of events
occurred, not when they occur.
• Superposition: The most basic concept used in relative
dating is the law of superposition. Simply stated, each
bed in a sequence of sedimentary rocks (or layered
volcanic rocks) is younger than the bed below it and
older than the bed above it. This law follows two basic
assumptions: (1) the beds were originally deposited
near horizontal, and (2) the beds were not overturned
after their deposition.
• Faunal Succession: Similar to the law of superposition is
the law of faunal succession, which states that groups of
fossil animals and plants occur throughout the
geologic record in a distinct and identifiable order.
Following this law, sedimentary rocks can be "dated"
by their characteristic fossil content. Particularly useful
are index fossils, geographically widespread fossils that
evolved rapidly through time.
Crosscutting Relationships: Relative ages of rocks and
events may also be determined using the law of
crosscutting relationships, which states that geologic
features such as igneous intrusions or faults are
younger than the units they cut across.
Inclusions: Inclusions, which are fragments of older
rock within a younger igneous rock or coarse-grained
sedimentary rock, also facilitate relative dating.
Inclusions are useful at contacts with igneous rock
bodies where magma moving upward through the
crust has dislodged and engulfed pieces of the older
surrounding rock.
Determining Relative Age
• Extrusion—it’s a lava hardens on the
surface . It’s younger than the rocks
below it.
• Intrusion—magma cools and hardens
into a mass of igneous rock. It is always
younger than the rock layers around
and beneath or it can be determined
that the igneous intrusion is younger
than the sedimentary rock.
Absolute dating is the process of
determining a specific date for an
archaeological or paleontological
site or artifact or knowing exactly
how old a rock layer is.
♥Absolute dates do not necessarily
tell us when a particular cultural
event happened, but when taken as
part of the overall archaeological
record they are invaluable in
constructing a more specific
sequence of events.
Determine the Absolute Age
Potassium-Argon Dating-- Potassium is common
in rocks and minerals Potassium-40 is a
radioactive isotope of potassium that decays into
argon-40. The half-life of potassium-40 is 1.3
billion years, far longer than that of carbon-14,
allowing much older samples to be dated.
Carbon-14 Dating--Sediments less than about
50,000 years old that contain organic material can
be dated based on the radioactive decay of the
isotope Carbon 14.
For example, shells, wood, and other material
found in the shoreline deposits of Utah's
prehistoric Lake Bonneville have yielded absolute
dates using this method.
William Smith
• discovered regular order of occurrence of fossils in rock layers.
While digging the Somerset Coal Canal in southwest England, he
found that fossils were always in the same order in the rock layers.
• As he continued his job as a surveyor, he found the same patterns
across England.
• He also found that certain animals were in only certain layers and
that they were in the same layers all across England.
• Due to that discovery, Smith was able to recognize the order that
the rocks were formed.
• Sixteen years after his discovery, he published a geological map of
England showing the rocks of different geologic time eras.
Planetesimal Hypothesis
• Planetesimal—any of innumerable small bodies
of accreted gas and dust thought to have orbited
the Sun during the formation of the
planets. These are solid objects thought to exist
in protoplanetary disks and in debris disks.
• Planetesimal hypothesis—hypothesis that the
planets and satellites of the solar system were
formed by gravitational aggregation of
planetesimals.
Planetesimal hypothesis
• Geologist Chamberline and astronomer
Moulton in early 20th century at the
University of Chicago.
• There hypothesis called for close passage
of another star past our sun.
• The pull of the intruder’s gravity field
presumably extracted solar gaseous
materials, which 1st condensed in space to
form small bodies called planetesimals.
The countless numbers of these cold
asteroid like bodies tens to hundreds of
kilometer in diameter aggregated to
form planets. As the planets grew, their
strengthening gravity fields attracted
still more particles.
Tertiary planets—Mercury, Venus,
Earth and Mars.
Jovian Planets—Jupiter,Saturn,
Uranus and Neptune
•The planets evolved from a cloud of
planetesimals which revolved around the sun.
♥The planetesimals, the tiny cosmic
fragments collided with each other and
united together to form larger bodies which
became planets and satellites revolving
around the sun. This idea was that of a solid
origin of the earth and the other planet and
satellites to start with. During the near-
collision, hot gases were pulled out of both
stars and the gases then condensed.
♦the planetesimals formed within a spiral disk
of dust and gas surrounding a central nucleus.
♦Their gravitational attraction eventually
caused the planetesimals to coalesce into
protoplanetary disks from which larger
objects such as planets, asteroids, and satellites
were formed, while the nucleus coalesced into
the Sun.
• Viktor Safronov
—his planetary hypothesis states that
planets form out of dust grains that
collide and stick to form larger and
larger bodies.
When the bodies reach sizes of
approximately one kilometer, then they
can attract each other directly through
their mutual gravity, aiding further
growth into moon-sized protoplanets
enormously.
End..

More Related Content

What's hot

Endogenic processes - The Process Within
Endogenic processes - The Process WithinEndogenic processes - The Process Within
Endogenic processes - The Process WithinRichie Jake Generale
 
Grade 11 Earth & Life Science (Earth System & Subsystems)
Grade 11 Earth & Life Science (Earth System & Subsystems)Grade 11 Earth & Life Science (Earth System & Subsystems)
Grade 11 Earth & Life Science (Earth System & Subsystems)Marileah Mendina
 
10. Earth's Interior Heat Notes
10. Earth's Interior Heat Notes10. Earth's Interior Heat Notes
10. Earth's Interior Heat Notesmgitterm
 
Solar System and its Origin)
Solar System and its Origin)Solar System and its Origin)
Solar System and its Origin)jun de la Ceruz
 
Physical science chapter1 for shs
Physical science chapter1 for shsPhysical science chapter1 for shs
Physical science chapter1 for shsJimnaira Abanto
 
physical science module 2 Q4.pptx
physical science module 2 Q4.pptxphysical science module 2 Q4.pptx
physical science module 2 Q4.pptxLucyGraceG
 
Deformation of Crust
Deformation of CrustDeformation of Crust
Deformation of CrustJerome Bigael
 
Earth and Life Science - Earth Subsystems
Earth and Life Science - Earth SubsystemsEarth and Life Science - Earth Subsystems
Earth and Life Science - Earth SubsystemsJuan Miguel Palero
 
Ancient Astronomy.pptx
Ancient Astronomy.pptxAncient Astronomy.pptx
Ancient Astronomy.pptxJaypeeFajardo1
 
MOVEMENT OF PLATES AND FORMATION OF FOLDS AND.pptx
MOVEMENT OF PLATES AND FORMATION OF  FOLDS AND.pptxMOVEMENT OF PLATES AND FORMATION OF  FOLDS AND.pptx
MOVEMENT OF PLATES AND FORMATION OF FOLDS AND.pptxmarionboyka
 
Origin of the Universe and the Solar System
 Origin of the Universe and the Solar System  Origin of the Universe and the Solar System
Origin of the Universe and the Solar System Donna Grace Herman
 
Geologic Processes on Earth
Geologic Processes on EarthGeologic Processes on Earth
Geologic Processes on EarthHanna Elise
 
Grade 11 Chapter 4 Module Earth Science : Water Resources
Grade 11 Chapter 4 Module Earth Science : Water ResourcesGrade 11 Chapter 4 Module Earth Science : Water Resources
Grade 11 Chapter 4 Module Earth Science : Water Resourcesyeshynegarin
 
Convection currents and the mantle powerpoint
Convection currents and the mantle powerpointConvection currents and the mantle powerpoint
Convection currents and the mantle powerpointkristannsnyder
 
Exogenic Processes
Exogenic ProcessesExogenic Processes
Exogenic ProcessesJonalyn Asi
 
Sea floor spreading
Sea floor spreadingSea floor spreading
Sea floor spreadingJenny Dixon
 
Earth and Life Science - Grade 11 (Minerals)
Earth and Life Science - Grade 11 (Minerals)Earth and Life Science - Grade 11 (Minerals)
Earth and Life Science - Grade 11 (Minerals)Love Ricarto
 
grade 11 chapter 4 module Earth Science: Water Resources
grade 11 chapter 4 module Earth Science: Water Resourcesgrade 11 chapter 4 module Earth Science: Water Resources
grade 11 chapter 4 module Earth Science: Water ResourcesRinaVeronicaFabian
 

What's hot (20)

Earth Subsystem
Earth SubsystemEarth Subsystem
Earth Subsystem
 
Endogenic processes - The Process Within
Endogenic processes - The Process WithinEndogenic processes - The Process Within
Endogenic processes - The Process Within
 
Grade 11 Earth & Life Science (Earth System & Subsystems)
Grade 11 Earth & Life Science (Earth System & Subsystems)Grade 11 Earth & Life Science (Earth System & Subsystems)
Grade 11 Earth & Life Science (Earth System & Subsystems)
 
10. Earth's Interior Heat Notes
10. Earth's Interior Heat Notes10. Earth's Interior Heat Notes
10. Earth's Interior Heat Notes
 
Solar System and its Origin)
Solar System and its Origin)Solar System and its Origin)
Solar System and its Origin)
 
Physical science chapter1 for shs
Physical science chapter1 for shsPhysical science chapter1 for shs
Physical science chapter1 for shs
 
physical science module 2 Q4.pptx
physical science module 2 Q4.pptxphysical science module 2 Q4.pptx
physical science module 2 Q4.pptx
 
Deformation of Crust
Deformation of CrustDeformation of Crust
Deformation of Crust
 
Earth and Life Science - Earth Subsystems
Earth and Life Science - Earth SubsystemsEarth and Life Science - Earth Subsystems
Earth and Life Science - Earth Subsystems
 
Ancient Astronomy.pptx
Ancient Astronomy.pptxAncient Astronomy.pptx
Ancient Astronomy.pptx
 
MOVEMENT OF PLATES AND FORMATION OF FOLDS AND.pptx
MOVEMENT OF PLATES AND FORMATION OF  FOLDS AND.pptxMOVEMENT OF PLATES AND FORMATION OF  FOLDS AND.pptx
MOVEMENT OF PLATES AND FORMATION OF FOLDS AND.pptx
 
Origin of the Universe and the Solar System
 Origin of the Universe and the Solar System  Origin of the Universe and the Solar System
Origin of the Universe and the Solar System
 
Geologic Processes on Earth
Geologic Processes on EarthGeologic Processes on Earth
Geologic Processes on Earth
 
Exogenous processes on earth
Exogenous processes on earthExogenous processes on earth
Exogenous processes on earth
 
Grade 11 Chapter 4 Module Earth Science : Water Resources
Grade 11 Chapter 4 Module Earth Science : Water ResourcesGrade 11 Chapter 4 Module Earth Science : Water Resources
Grade 11 Chapter 4 Module Earth Science : Water Resources
 
Convection currents and the mantle powerpoint
Convection currents and the mantle powerpointConvection currents and the mantle powerpoint
Convection currents and the mantle powerpoint
 
Exogenic Processes
Exogenic ProcessesExogenic Processes
Exogenic Processes
 
Sea floor spreading
Sea floor spreadingSea floor spreading
Sea floor spreading
 
Earth and Life Science - Grade 11 (Minerals)
Earth and Life Science - Grade 11 (Minerals)Earth and Life Science - Grade 11 (Minerals)
Earth and Life Science - Grade 11 (Minerals)
 
grade 11 chapter 4 module Earth Science: Water Resources
grade 11 chapter 4 module Earth Science: Water Resourcesgrade 11 chapter 4 module Earth Science: Water Resources
grade 11 chapter 4 module Earth Science: Water Resources
 

Similar to Tidal Theory

Module 1 origin and systems of earth
Module 1 origin and systems of earthModule 1 origin and systems of earth
Module 1 origin and systems of earthbrionesako
 
Age of the Earth LCTV
Age of the Earth LCTVAge of the Earth LCTV
Age of the Earth LCTVBill Vales
 
The earth’s interior
The earth’s interiorThe earth’s interior
The earth’s interiorjnr
 
Environmental studies notes for Marine students
Environmental studies notes for Marine studentsEnvironmental studies notes for Marine students
Environmental studies notes for Marine studentsCaptMadanKumar
 
Geology Complete (Earth Science Topic)
Geology Complete (Earth Science Topic)Geology Complete (Earth Science Topic)
Geology Complete (Earth Science Topic)Avigail Gabaleo Maximo
 
Earth in space
Earth in spaceEarth in space
Earth in spaceTEWABE
 
3 types of tectonics plate
3 types of tectonics plate3 types of tectonics plate
3 types of tectonics plateslash dhan
 
Origin of the universe
Origin of the universe Origin of the universe
Origin of the universe Shella69
 
Historyoftheearth
HistoryoftheearthHistoryoftheearth
Historyoftheearthmartagar78
 
nla.news-article130570301.3.pdf
nla.news-article130570301.3.pdfnla.news-article130570301.3.pdf
nla.news-article130570301.3.pdfBraydenStoch2
 
Geography class 11(Fundamentals of Physical Geography)
Geography class 11(Fundamentals of Physical Geography) Geography class 11(Fundamentals of Physical Geography)
Geography class 11(Fundamentals of Physical Geography) Shivam Kapri
 
Earth and life Science (Origin of the Universe and Star System, Earth System,...
Earth and life Science (Origin of the Universe and Star System, Earth System,...Earth and life Science (Origin of the Universe and Star System, Earth System,...
Earth and life Science (Origin of the Universe and Star System, Earth System,...Jerry Taay
 

Similar to Tidal Theory (20)

Module 1 origin and systems of earth
Module 1 origin and systems of earthModule 1 origin and systems of earth
Module 1 origin and systems of earth
 
Age of the Earth LCTV
Age of the Earth LCTVAge of the Earth LCTV
Age of the Earth LCTV
 
(1)origin of earth.ppt
(1)origin of earth.ppt(1)origin of earth.ppt
(1)origin of earth.ppt
 
Lesson 1.3
Lesson 1.3Lesson 1.3
Lesson 1.3
 
The earth’s interior
The earth’s interiorThe earth’s interior
The earth’s interior
 
Environmental studies notes for Marine students
Environmental studies notes for Marine studentsEnvironmental studies notes for Marine students
Environmental studies notes for Marine students
 
Geology Complete (Earth Science Topic)
Geology Complete (Earth Science Topic)Geology Complete (Earth Science Topic)
Geology Complete (Earth Science Topic)
 
Earth in space
Earth in spaceEarth in space
Earth in space
 
GEO610 Module I.pdf
GEO610 Module I.pdfGEO610 Module I.pdf
GEO610 Module I.pdf
 
introduction of Earth
introduction of Earthintroduction of Earth
introduction of Earth
 
3 types of tectonics plate
3 types of tectonics plate3 types of tectonics plate
3 types of tectonics plate
 
movements in the earth
movements in the earthmovements in the earth
movements in the earth
 
Solar system
Solar systemSolar system
Solar system
 
Origin of the universe
Origin of the universe Origin of the universe
Origin of the universe
 
Geo Proj
Geo ProjGeo Proj
Geo Proj
 
Historyoftheearth
HistoryoftheearthHistoryoftheearth
Historyoftheearth
 
nla.news-article130570301.3.pdf
nla.news-article130570301.3.pdfnla.news-article130570301.3.pdf
nla.news-article130570301.3.pdf
 
Geography class 11(Fundamentals of Physical Geography)
Geography class 11(Fundamentals of Physical Geography) Geography class 11(Fundamentals of Physical Geography)
Geography class 11(Fundamentals of Physical Geography)
 
Earthquake
EarthquakeEarthquake
Earthquake
 
Earth and life Science (Origin of the Universe and Star System, Earth System,...
Earth and life Science (Origin of the Universe and Star System, Earth System,...Earth and life Science (Origin of the Universe and Star System, Earth System,...
Earth and life Science (Origin of the Universe and Star System, Earth System,...
 

More from Google, Facebook, Twitter, Hotmail

Suggested answers to frequently asked questions in a job interview
Suggested answers to frequently asked questions in a job interviewSuggested answers to frequently asked questions in a job interview
Suggested answers to frequently asked questions in a job interviewGoogle, Facebook, Twitter, Hotmail
 

More from Google, Facebook, Twitter, Hotmail (20)

Whole language
Whole languageWhole language
Whole language
 
Suggested answers to frequently asked questions in a job interview
Suggested answers to frequently asked questions in a job interviewSuggested answers to frequently asked questions in a job interview
Suggested answers to frequently asked questions in a job interview
 
Interview for applying a job
Interview for applying a jobInterview for applying a job
Interview for applying a job
 
Resume writing
Resume writingResume writing
Resume writing
 
Competency-based language teaching
Competency-based language teachingCompetency-based language teaching
Competency-based language teaching
 
Oral Approach and Situational
Oral Approach and SituationalOral Approach and Situational
Oral Approach and Situational
 
The Nature of Approaches and Methods in Language
The Nature of Approaches and Methods in LanguageThe Nature of Approaches and Methods in Language
The Nature of Approaches and Methods in Language
 
Syllabus
SyllabusSyllabus
Syllabus
 
The Audiolingual Method
The Audiolingual MethodThe Audiolingual Method
The Audiolingual Method
 
Cells
CellsCells
Cells
 
Tsunami
TsunamiTsunami
Tsunami
 
Bacteria
BacteriaBacteria
Bacteria
 
Microbiology
Microbiology Microbiology
Microbiology
 
Surface Water
Surface WaterSurface Water
Surface Water
 
Aquifer
AquiferAquifer
Aquifer
 
Kingdom Animalia
Kingdom AnimaliaKingdom Animalia
Kingdom Animalia
 
Dam Construction
Dam ConstructionDam Construction
Dam Construction
 
Ground water extension and contamination
Ground water extension and contaminationGround water extension and contamination
Ground water extension and contamination
 
Bacterial Reproduction
Bacterial ReproductionBacterial Reproduction
Bacterial Reproduction
 
Clouds
CloudsClouds
Clouds
 

Recently uploaded

microwave assisted reaction. General introduction
microwave assisted reaction. General introductionmicrowave assisted reaction. General introduction
microwave assisted reaction. General introductionMaksud Ahmed
 
Grant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy ConsultingGrant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy ConsultingTechSoup
 
The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13Steve Thomason
 
fourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writingfourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writingTeacherCyreneCayanan
 
Measures of Dispersion and Variability: Range, QD, AD and SD
Measures of Dispersion and Variability: Range, QD, AD and SDMeasures of Dispersion and Variability: Range, QD, AD and SD
Measures of Dispersion and Variability: Range, QD, AD and SDThiyagu K
 
Class 11th Physics NEET formula sheet pdf
Class 11th Physics NEET formula sheet pdfClass 11th Physics NEET formula sheet pdf
Class 11th Physics NEET formula sheet pdfAyushMahapatra5
 
Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111Sapana Sha
 
Introduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The BasicsIntroduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The BasicsTechSoup
 
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptxSOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptxiammrhaywood
 
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in DelhiRussian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhikauryashika82
 
Paris 2024 Olympic Geographies - an activity
Paris 2024 Olympic Geographies - an activityParis 2024 Olympic Geographies - an activity
Paris 2024 Olympic Geographies - an activityGeoBlogs
 
Unit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptxUnit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptxVishalSingh1417
 
1029 - Danh muc Sach Giao Khoa 10 . pdf
1029 -  Danh muc Sach Giao Khoa 10 . pdf1029 -  Danh muc Sach Giao Khoa 10 . pdf
1029 - Danh muc Sach Giao Khoa 10 . pdfQucHHunhnh
 
Web & Social Media Analytics Previous Year Question Paper.pdf
Web & Social Media Analytics Previous Year Question Paper.pdfWeb & Social Media Analytics Previous Year Question Paper.pdf
Web & Social Media Analytics Previous Year Question Paper.pdfJayanti Pande
 
BAG TECHNIQUE Bag technique-a tool making use of public health bag through wh...
BAG TECHNIQUE Bag technique-a tool making use of public health bag through wh...BAG TECHNIQUE Bag technique-a tool making use of public health bag through wh...
BAG TECHNIQUE Bag technique-a tool making use of public health bag through wh...Sapna Thakur
 
1029-Danh muc Sach Giao Khoa khoi 6.pdf
1029-Danh muc Sach Giao Khoa khoi  6.pdf1029-Danh muc Sach Giao Khoa khoi  6.pdf
1029-Danh muc Sach Giao Khoa khoi 6.pdfQucHHunhnh
 
Beyond the EU: DORA and NIS 2 Directive's Global Impact
Beyond the EU: DORA and NIS 2 Directive's Global ImpactBeyond the EU: DORA and NIS 2 Directive's Global Impact
Beyond the EU: DORA and NIS 2 Directive's Global ImpactPECB
 

Recently uploaded (20)

microwave assisted reaction. General introduction
microwave assisted reaction. General introductionmicrowave assisted reaction. General introduction
microwave assisted reaction. General introduction
 
Grant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy ConsultingGrant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy Consulting
 
The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13
 
fourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writingfourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writing
 
Measures of Dispersion and Variability: Range, QD, AD and SD
Measures of Dispersion and Variability: Range, QD, AD and SDMeasures of Dispersion and Variability: Range, QD, AD and SD
Measures of Dispersion and Variability: Range, QD, AD and SD
 
Class 11th Physics NEET formula sheet pdf
Class 11th Physics NEET formula sheet pdfClass 11th Physics NEET formula sheet pdf
Class 11th Physics NEET formula sheet pdf
 
Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111
 
Introduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The BasicsIntroduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The Basics
 
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptxSOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
 
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in DelhiRussian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
 
Paris 2024 Olympic Geographies - an activity
Paris 2024 Olympic Geographies - an activityParis 2024 Olympic Geographies - an activity
Paris 2024 Olympic Geographies - an activity
 
Unit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptxUnit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptx
 
1029 - Danh muc Sach Giao Khoa 10 . pdf
1029 -  Danh muc Sach Giao Khoa 10 . pdf1029 -  Danh muc Sach Giao Khoa 10 . pdf
1029 - Danh muc Sach Giao Khoa 10 . pdf
 
Web & Social Media Analytics Previous Year Question Paper.pdf
Web & Social Media Analytics Previous Year Question Paper.pdfWeb & Social Media Analytics Previous Year Question Paper.pdf
Web & Social Media Analytics Previous Year Question Paper.pdf
 
BAG TECHNIQUE Bag technique-a tool making use of public health bag through wh...
BAG TECHNIQUE Bag technique-a tool making use of public health bag through wh...BAG TECHNIQUE Bag technique-a tool making use of public health bag through wh...
BAG TECHNIQUE Bag technique-a tool making use of public health bag through wh...
 
Mattingly "AI & Prompt Design: The Basics of Prompt Design"
Mattingly "AI & Prompt Design: The Basics of Prompt Design"Mattingly "AI & Prompt Design: The Basics of Prompt Design"
Mattingly "AI & Prompt Design: The Basics of Prompt Design"
 
1029-Danh muc Sach Giao Khoa khoi 6.pdf
1029-Danh muc Sach Giao Khoa khoi  6.pdf1029-Danh muc Sach Giao Khoa khoi  6.pdf
1029-Danh muc Sach Giao Khoa khoi 6.pdf
 
Código Creativo y Arte de Software | Unidad 1
Código Creativo y Arte de Software | Unidad 1Código Creativo y Arte de Software | Unidad 1
Código Creativo y Arte de Software | Unidad 1
 
Beyond the EU: DORA and NIS 2 Directive's Global Impact
Beyond the EU: DORA and NIS 2 Directive's Global ImpactBeyond the EU: DORA and NIS 2 Directive's Global Impact
Beyond the EU: DORA and NIS 2 Directive's Global Impact
 
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptxINDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
 

Tidal Theory

  • 1. Tidal Theory By: Jackelyn Diaz BSEd-Bio. Sci.II
  • 2. Tidal theory-- a theory of the evolution of a celestial body that is based on the action of tidal forces; specify : such a theory explaining the moon's evolution. It is the application of continuum mechanics to interpret and predict the tidal deformations of planetary and satellite bodies and their atmospheres and oceans, under the gravitational loading of another astronomical body or bodies. It commonly refers to the fluid dynamic motions for the Earth's oceans.
  • 3. Tides—motion caused by the gravitational attraction between the earth, moon and sun. Newton (Theory of Gravity)— tides are caused by a differential gravitational pull.
  • 4. Spring tides—sun, moon and earth are all aligned. The tides are high. It occurs twice a month during full moon and new moon. ♥The gravitational pull of the moon and sun are combined. At these times, the high tides are very high and the low tides are very low.
  • 5.
  • 6. Neap tides—moon and sun are at right angles to each other. Tidal extremes are reduced. It occurs during 1st and 3rd quarter of the moon.
  • 7.
  • 9. Relative Dating—It is the science determining the relative order of past events, without necessarily determining their absolute age. ♦It is when you know the age of a certain rock layer is by comparing the fossils. ♦It can only determine the sequential order in which a series of events occurred, not when they occur.
  • 10. • Superposition: The most basic concept used in relative dating is the law of superposition. Simply stated, each bed in a sequence of sedimentary rocks (or layered volcanic rocks) is younger than the bed below it and older than the bed above it. This law follows two basic assumptions: (1) the beds were originally deposited near horizontal, and (2) the beds were not overturned after their deposition. • Faunal Succession: Similar to the law of superposition is the law of faunal succession, which states that groups of fossil animals and plants occur throughout the geologic record in a distinct and identifiable order. Following this law, sedimentary rocks can be "dated" by their characteristic fossil content. Particularly useful are index fossils, geographically widespread fossils that evolved rapidly through time.
  • 11. Crosscutting Relationships: Relative ages of rocks and events may also be determined using the law of crosscutting relationships, which states that geologic features such as igneous intrusions or faults are younger than the units they cut across. Inclusions: Inclusions, which are fragments of older rock within a younger igneous rock or coarse-grained sedimentary rock, also facilitate relative dating. Inclusions are useful at contacts with igneous rock bodies where magma moving upward through the crust has dislodged and engulfed pieces of the older surrounding rock.
  • 12. Determining Relative Age • Extrusion—it’s a lava hardens on the surface . It’s younger than the rocks below it. • Intrusion—magma cools and hardens into a mass of igneous rock. It is always younger than the rock layers around and beneath or it can be determined that the igneous intrusion is younger than the sedimentary rock.
  • 13. Absolute dating is the process of determining a specific date for an archaeological or paleontological site or artifact or knowing exactly how old a rock layer is. ♥Absolute dates do not necessarily tell us when a particular cultural event happened, but when taken as part of the overall archaeological record they are invaluable in constructing a more specific sequence of events.
  • 14. Determine the Absolute Age Potassium-Argon Dating-- Potassium is common in rocks and minerals Potassium-40 is a radioactive isotope of potassium that decays into argon-40. The half-life of potassium-40 is 1.3 billion years, far longer than that of carbon-14, allowing much older samples to be dated. Carbon-14 Dating--Sediments less than about 50,000 years old that contain organic material can be dated based on the radioactive decay of the isotope Carbon 14. For example, shells, wood, and other material found in the shoreline deposits of Utah's prehistoric Lake Bonneville have yielded absolute dates using this method.
  • 15. William Smith • discovered regular order of occurrence of fossils in rock layers. While digging the Somerset Coal Canal in southwest England, he found that fossils were always in the same order in the rock layers. • As he continued his job as a surveyor, he found the same patterns across England. • He also found that certain animals were in only certain layers and that they were in the same layers all across England. • Due to that discovery, Smith was able to recognize the order that the rocks were formed. • Sixteen years after his discovery, he published a geological map of England showing the rocks of different geologic time eras.
  • 16. Planetesimal Hypothesis • Planetesimal—any of innumerable small bodies of accreted gas and dust thought to have orbited the Sun during the formation of the planets. These are solid objects thought to exist in protoplanetary disks and in debris disks. • Planetesimal hypothesis—hypothesis that the planets and satellites of the solar system were formed by gravitational aggregation of planetesimals.
  • 17. Planetesimal hypothesis • Geologist Chamberline and astronomer Moulton in early 20th century at the University of Chicago. • There hypothesis called for close passage of another star past our sun. • The pull of the intruder’s gravity field presumably extracted solar gaseous materials, which 1st condensed in space to form small bodies called planetesimals.
  • 18. The countless numbers of these cold asteroid like bodies tens to hundreds of kilometer in diameter aggregated to form planets. As the planets grew, their strengthening gravity fields attracted still more particles. Tertiary planets—Mercury, Venus, Earth and Mars. Jovian Planets—Jupiter,Saturn, Uranus and Neptune
  • 19. •The planets evolved from a cloud of planetesimals which revolved around the sun. ♥The planetesimals, the tiny cosmic fragments collided with each other and united together to form larger bodies which became planets and satellites revolving around the sun. This idea was that of a solid origin of the earth and the other planet and satellites to start with. During the near- collision, hot gases were pulled out of both stars and the gases then condensed.
  • 20. ♦the planetesimals formed within a spiral disk of dust and gas surrounding a central nucleus. ♦Their gravitational attraction eventually caused the planetesimals to coalesce into protoplanetary disks from which larger objects such as planets, asteroids, and satellites were formed, while the nucleus coalesced into the Sun.
  • 21. • Viktor Safronov —his planetary hypothesis states that planets form out of dust grains that collide and stick to form larger and larger bodies. When the bodies reach sizes of approximately one kilometer, then they can attract each other directly through their mutual gravity, aiding further growth into moon-sized protoplanets enormously.
  • 22. End..