The document discusses the theory of planetesimals to explain the formation of the solar system and Earth. It describes how:
1) A gas and dust nebula received an expansive wave from a supernova, causing it to rotate and collapse into a disk with matter accumulating in the center to form our sun.
2) Planetesimals formed as small bits of matter collided and joined together, eventually creating the planets. The outer planets attracted gas to become gas giants, while inner planets like Earth took longer to form and remained smaller without gas.
3) Earth underwent multiple events since forming 4.6 billion years ago, allowing its history to be divided into eons such as the Hadean, Arche
Planetary Vacuums, Atmospheres, & LifePaul H. Carr
While does our earth have a 21% Oxygen Atmosphere,
when our neighboring planets, Mars, and Venus, have mostly Carbon Dioxide?
Could our earth have a runaway greenhouse effect like Venus?
Is there life on the billions of exo-planets?
Maybe too in-depth for most elementary students, but very good broad coverage for teacher background or more advanced students in elementary or middle school.
This presentations covers composition of air ,layers of atmosphere.If you like this presentation please give it a like .
for more interesting presentations visit my page - http://allfactsatonce.blogspot.in/
Planetary Vacuums, Atmospheres, & LifePaul H. Carr
While does our earth have a 21% Oxygen Atmosphere,
when our neighboring planets, Mars, and Venus, have mostly Carbon Dioxide?
Could our earth have a runaway greenhouse effect like Venus?
Is there life on the billions of exo-planets?
Maybe too in-depth for most elementary students, but very good broad coverage for teacher background or more advanced students in elementary or middle school.
This presentations covers composition of air ,layers of atmosphere.If you like this presentation please give it a like .
for more interesting presentations visit my page - http://allfactsatonce.blogspot.in/
The divergent fates of primitive hydrospheric water on Earth and MarsSérgio Sacani
Despite active transport into Earth’s mantle, water has been
present on our planet’s surface for most of geological time1,2
.
Yet water disappeared from the Martian surface soon after its
formation. Although some of the water on Mars was lost to space
via photolysis following the collapse of the planet’s magnetic field3–5,
the widespread serpentinization of Martian crust6,7
suggests that
metamorphic hydration reactions played a critical part in the
sequestration of the crust. Here we quantify the relative volumes
of water that could be removed from each planet’s surface via the
burial and metamorphism of hydrated mafic crusts, and calculate
mineral transition-induced bulk-density changes at conditions
of elevated pressure and temperature for each. The metamorphic
mineral assemblages in relatively FeO-rich Martian lavas can
hold about 25 per cent more structurally bound water than those
in metamorphosed terrestrial basalts, and can retain it at greater
depths within Mars. Our calculations suggest that in excess of
9 per cent by volume of the Martian mantle may contain hydrous
mineral species as a consequence of surface reactions, compared to
about 4 per cent by volume of Earth’s mantle. Furthermore, neither
primitive nor evolved hydrated Martian crust show noticeably
different bulk densities compared to their anhydrous equivalents,
in contrast to hydrous mafic terrestrial crust, which transforms
to denser eclogite upon dehydration. This would have allowed
efficient overplating and burial of early Martian crust in a stagnantlid
tectonic regime, in which the lithosphere comprised a single
tectonic plate, with only the warmer, lower crust involved in mantle
convection. This provided an important sink for hydrospheric water
and a mechanism for oxidizing the Martian mantle. Conversely,
relatively buoyant mafic crust and hotter geothermal gradients on
Earth reduced the potential for upper-mantle hydration early in
its geological history, leading to water being retained close to its
surface, and thus creating conditions conducive for the evolution
of complex multicellular life
TEMA 6 VAMOS AL LÍO.BIOLOGÍA Y GEOLOGÍApptxsalowil
APARATO REPRODUCTOS MASCULINO Y FEMENINO, LOS GAMETOS, FECUNDACIÓN IN VITRO, FASES DEL EMBARAZO, MÉTODOS ANTICONCEPTIVOS, LIBERTAD DE SEXUALIDAD Y DE GÉNERO.
UNIDAD 5 INNOVACIONES MÉDICAS. CULTURA CIENTIFICApptxsalowil
EVOLUCIÓN DE LOS TÉRMINOS SALUD Y ENFERMEDAD, TIPOS DE ENFERMEDADES, DIAGNÓSTICO, PREVENCIÓN Y CURACIÓN. ENFERMEDADES DE NUESTRO TIEMPO, TIPOS DE DROGAS, ÚLTIMOS AVANCES EN BIOMEDICINA
DIFERENCIA ENTRE ALIMENTACIÓN Y NUTRICIÓN. PRINCIPALES NUTRIENTES. RUEDA DE LOS ALIMENTOS. DIETA MEDITERRÁNEA. ENFERMEDADES Y PARÁSITOS RELACIONADOS CON LA ALIMENTACIÓN.
We all have good and bad thoughts from time to time and situation to situation. We are bombarded daily with spiraling thoughts(both negative and positive) creating all-consuming feel , making us difficult to manage with associated suffering. Good thoughts are like our Mob Signal (Positive thought) amidst noise(negative thought) in the atmosphere. Negative thoughts like noise outweigh positive thoughts. These thoughts often create unwanted confusion, trouble, stress and frustration in our mind as well as chaos in our physical world. Negative thoughts are also known as “distorted thinking”.
Welcome to TechSoup New Member Orientation and Q&A (May 2024).pdfTechSoup
In this webinar you will learn how your organization can access TechSoup's wide variety of product discount and donation programs. From hardware to software, we'll give you a tour of the tools available to help your nonprofit with productivity, collaboration, financial management, donor tracking, security, and more.
How to Create Map Views in the Odoo 17 ERPCeline George
The map views are useful for providing a geographical representation of data. They allow users to visualize and analyze the data in a more intuitive manner.
Ethnobotany and Ethnopharmacology:
Ethnobotany in herbal drug evaluation,
Impact of Ethnobotany in traditional medicine,
New development in herbals,
Bio-prospecting tools for drug discovery,
Role of Ethnopharmacology in drug evaluation,
Reverse Pharmacology.
Students, digital devices and success - Andreas Schleicher - 27 May 2024..pptxEduSkills OECD
Andreas Schleicher presents at the OECD webinar ‘Digital devices in schools: detrimental distraction or secret to success?’ on 27 May 2024. The presentation was based on findings from PISA 2022 results and the webinar helped launch the PISA in Focus ‘Managing screen time: How to protect and equip students against distraction’ https://www.oecd-ilibrary.org/education/managing-screen-time_7c225af4-en and the OECD Education Policy Perspective ‘Students, digital devices and success’ can be found here - https://oe.cd/il/5yV
Read| The latest issue of The Challenger is here! We are thrilled to announce that our school paper has qualified for the NATIONAL SCHOOLS PRESS CONFERENCE (NSPC) 2024. Thank you for your unwavering support and trust. Dive into the stories that made us stand out!
Operation “Blue Star” is the only event in the history of Independent India where the state went into war with its own people. Even after about 40 years it is not clear if it was culmination of states anger over people of the region, a political game of power or start of dictatorial chapter in the democratic setup.
The people of Punjab felt alienated from main stream due to denial of their just demands during a long democratic struggle since independence. As it happen all over the word, it led to militant struggle with great loss of lives of military, police and civilian personnel. Killing of Indira Gandhi and massacre of innocent Sikhs in Delhi and other India cities was also associated with this movement.
The Indian economy is classified into different sectors to simplify the analysis and understanding of economic activities. For Class 10, it's essential to grasp the sectors of the Indian economy, understand their characteristics, and recognize their importance. This guide will provide detailed notes on the Sectors of the Indian Economy Class 10, using specific long-tail keywords to enhance comprehension.
For more information, visit-www.vavaclasses.com
2. ORIGIN OF THE SOLAR SYSTEM
THE CURRENTLY ACCEPTED THEORY TO EXPLAIN THE FORMATION OF THE
SOLAR SYSTEM, AND THE OWN EARTH IS THE THEORY OF THE
PLANETESIMALS:
1. A GAS AND DUST NEBULA, FLOATING IN SPACE WITH VERY SLOW
MOVEMENTS BETWEEN ITS PARTICLES TILL IT RECEIVED THE EXPANSIVE
WAVE OF THE EXPLOSION OF A NEARBY SUPERNOVA.
2. THE NEBULA BEGAN TO ROTATE MUCH FASTER, AND TO COLLAPSE IN A
SINGLE PLANE.
3. IN THE CENTER OF THE NEBULA, THE ACCUMULATION OF MATTER AND
THE CONTINUOUS SHOOTS INCREASED THE PRESSURE AND THE
TEMPERATURE, ALLOWING THAT THEY WILL BEGIN TO NUCLEAR
REACTIONS. THAT WAS BORN OUR SUN FROM A PROTOSOL.
3. ORIGIN OF THE SOLAR SYSTEM
4. OUR CENTRAL STAR ATTRACTED 99.85% OF THE MATTER AND GAS OF
THE SYSTEM, BUT THE REST WAS ABLE TO SEPARATE AND THROUGH
THE ROCK LINE, WHERE THERE WAS PIECE OF MATTER AND EVEN
FURTHER, AFTER THE FREEZING LINE GASES WERE SOLIDIFIED AS
WATER VAPOR, METHANE, ETC.
5. SMALL BITS OF MATTER, THEY WOULD BEGIN TO COLLIDE WITH LITTLE
VIOLENCE AND JOIN IN AGGREGATES OF GREATER SIZE CALLS
PLANETESIMALS, WHICH WOULD IMPACT THEMSELVES, INCREASING
SIZE UNTIL FORMING THE PLANETS.
6. THIS PROCESS WAS FASTER IN THE FORMATION OF THE EXTERNAL
PLANETS BECAUSE THERE WERE MUCH MORE GREAT AMOUNT OF
FLOATING PARTICLES. ONCE THESE PLANETS REACH A DETERMINED
SIZE, THEY BEGIN TO ATTRACT THE GAS AND MATTER THAT SURROUND
THEMSELVES WITH GRAVITATORY FORCES, BECOMING GASEOUS
GIANTS (EXTERNAL PLANETS).
4. ORIGIN OF THE SOLAR SYSTEM
7. IN THE AREA LOCATED BETWEEN THE ROCK LINE AND THE FREEZING
LINE, WHEN THE TEMPERATURE IS GREATER, GAS IS SCARCE AND THE
ROCK PARTICLES IN SUSPENSION ARE LESS ABUNDANT, SO THAT IT
TAKES MUCH MORE TIME TO FORM THE PLANETS FROM
PLANETESIMALS. IN ADDITION TO THE NO GAS, THERE CAN ONLY
ATTRACT ROCK FRAGMENTS, SO THE INTERIOR PLANETS WILL BE LESS
SIZE THAN THE EXTERNAL PLANETS.
8. THE EARTH IN ITS FIRST STAGES WAS ACCOMPANIED BY ANOTHER
PROTOPLANET CALLED CEIA, FINALLY COLLISED, WINNING THE EARTH
MASS AND A MOON. FINALLY 4500 M.A. AGO, THE EARTH IS STABILIZED
AND BECOMES ONE OF THE INTERNAL PLANETS.
5. ORIGIN OF THE SOLAR SYSTEM
7. IN THE AREA LOCATED BETWEEN THE ROCK LINE AND THE FREEZING
LINE, WHEN THE TEMPERATURE IS GREATER, GAS IS SCARCE AND THE
ROCK PARTICLES IN SUSPENSION ARE LESS ABUNDANT, SO THAT IT
TAKES MUCH MORE TIME TO FORM THE PLANETS FROM
PLANETESIMALS. IN ADDITION TO THE NO GAS, THERE CAN ONLY
ATTRACT ROCK FRAGMENTS, SO THE INTERIOR PLANETS WILL BE LESS
SIZE THAN THE EXTERNAL PLANETS.
8. THE EARTH IN ITS FIRST STAGES WAS ACCOMPANIED BY ANOTHER
PROTOPLANET CALLED CEIA, FINALLY COLLISED, WINNING THE EARTH
MASS AND A MOON. FINALLY 4500 M.A. AGO, THE EARTH IS STABILIZED
AND BECOMES ONE OF THE INTERNAL PLANETS.
6. THE HISTORY OF THE EARTH
• SINCE ITS FORMATION 4600 M.A. AGO MULTITUDE OF EVENTS ON THE
EARTH
HAS HAPPENED, WHICH HAS ALLOWED TO FRACTION TIME IN EONS, ERAS
AND
PERIODS FOR ITS BEST STUDY. CURRENTLY 4 EONS ARE RECOGNIZED:
1. HADIC EON (4500-3600 M.a.)
2. ARCHAIC EON (3600-2500 M.a.)
3. PROTEROZOIC EON (2500-540 M.a.)
4. FANEROZOIC EON (540-NOW)
7. HADIC EON
CALLED IN HONOR TO HADES, HELL IN GREEK MYTHOLOGY, DUE TO THE
CONDITIONS OF THE EARTH DURING THIS TIME. THE EARTH IS IN ITS
FORMATION PHASE, METEORITES FALL CONTINUOUSLY INCREASING ITS
TEMPERATURE, BEING INITIALLY AN AUTHENTIC SEA OF LAVA TO MORE THAN
1000º C.
THE EARTH BEGINS TO COOL AND A VERY UNSTABLE SOLID BARK IS
FORMED, BECAUSE IT IS ON A FUNDED LAYER AND THE IMPACT OF
METEORITES. GASES RELEASED FROM THE LAVA WILL GENERATE THE
ATMOSPHERE (RICH IN CO2 AND WATER VAPOR) AND THE HYDROSPHERE.
THE OLDEST ROCKS FORMED AT THE END OF THIS STAGE, 3600 M.a. AGO.
9. HADIC EON
THE APPEARANCE OF WATER ON THE EARTH IS A MYSTERY
STILL, IT IS CURRENTLY BELIEVED THAT MOST OF THE WATER
ARRIVED IN ASTEROIDS AND COMETS WITH HIGH CONTENT IN
WATER THAT COLLIDED WITH THE EARTH IN FORMATION. THIS
WATER WAS EVAPORATED ON THE SURFACE, AND THE
WATER VAPOR ASCENDED IN IMMENSE AMOUNTS FORMING
THICK CLOUDS, TRIGGING A HUGE DILUVIUM THAT LAST
MILLION YEARS.
10. ARCHAIC EON
GEOLOGY: THE FIRST ROCKS ARE METAMORFICAL OR
VOLCANIC, WHILE THE ATMOSPHERE IS FORMED BY
METHANE (CH4) CARBON DIOXIDE (CO2) AND AMMONIA (NH3).
WEATHER: THE SUN IRRADIAED LESS ENERGY THAN NOW,
HOWEVER, THE TEMPERATURE WAS ABOUT 30 ° C ON THE
SURFACE AND BETWEEN 30-40 ° C IN THE OCEAN DUE TO THE
GREAT GREENHOUSE EFFECT OF THE CO2 RICH
ATMOSPHERE.
LIFE: THE FIRST LIVING BEINGS CAME UP 3500 M.a. AGO. THEY
WERE PROCARIOTS CELLS, FILAMENT BACTERIA LIVING IN
THE ARCHAIC OCEANS. THE PHOTOSYNTHESIS PROCESS
COMES UP AND THE ATMOSPHERE ENRICHES IN O2.