The document summarizes key features of continental margins and ocean basins. Continental margins have three divisions: continental shelves, slopes, and rises. Shelves gently slope away from land and are composed of continental crust. Slopes more steeply slope from shelves into ocean basins. Rises are found at the base of slopes and accumulate sediment. Margins are either passive with thick sediment or active with thin sediment at convergent plate boundaries. Ocean basins cover 30% of Earth and contain abyssal plains, trenches, ridges, and seamounts.
The reason for the occurrence of such a huge mass of water on the globe, is still a myth and reality. The reason goes back to the Origin of Earth itself. The exact mode of origin is not precisely known. Scientists assume, both Primary and secondary sources would have given rise to all both air and water on the earth. Two possible sources as internal source (or) external source have been proposed so far. Some of them are attributed towards the theories of origin of the earth.
Boundary problems between :-
Precambrian/Cambrian
Permian/Triassic
Cretaceous/Tertiary
Neogene/Quaternary
Stratigraphic boundaries are determined by one or more of geological events such as volcanic activity, sedimentation, tectonism, paleo-environments & evolution of life.
Faunal records have played major role in determining the boundaries of the Phanerozoic units.
The other geological events are dated on the evidence of fossil records.
Oceanography is an interesting subject. Geological oceanography deals with a lot of unique aspects of the oceans including the ocean morphology and relief, continental margins, tectonic processes acting on the ocean bottoms, marine mineral resources, and the deep sea deposits. The subject also focuses on the never ending dynamic processes like ocean waters, ocean currents and their impacts with reference to space and time. Understanding the tectonic disposition and movement of crustal plates are an important part while studying the earth and atmospheric sciences, in general and oceanography, in particular. The continental margins and the deep ocean basins are the two major aspects to be understood in this subject. This lesson is on the characteristics of continental margins.
Sedimentary basins are the depressions in the earth's crust where loose particles accumulate and finally lithified to form sedimentary rocks. Basins are particularly attractive to geoscientists from time immemorial due to the wealth hidden here in the form of oil, gas, coal etc. In this document you will find the types of basins, basin-fill types, methods of basin analysis and so on.
The reason for the occurrence of such a huge mass of water on the globe, is still a myth and reality. The reason goes back to the Origin of Earth itself. The exact mode of origin is not precisely known. Scientists assume, both Primary and secondary sources would have given rise to all both air and water on the earth. Two possible sources as internal source (or) external source have been proposed so far. Some of them are attributed towards the theories of origin of the earth.
Boundary problems between :-
Precambrian/Cambrian
Permian/Triassic
Cretaceous/Tertiary
Neogene/Quaternary
Stratigraphic boundaries are determined by one or more of geological events such as volcanic activity, sedimentation, tectonism, paleo-environments & evolution of life.
Faunal records have played major role in determining the boundaries of the Phanerozoic units.
The other geological events are dated on the evidence of fossil records.
Oceanography is an interesting subject. Geological oceanography deals with a lot of unique aspects of the oceans including the ocean morphology and relief, continental margins, tectonic processes acting on the ocean bottoms, marine mineral resources, and the deep sea deposits. The subject also focuses on the never ending dynamic processes like ocean waters, ocean currents and their impacts with reference to space and time. Understanding the tectonic disposition and movement of crustal plates are an important part while studying the earth and atmospheric sciences, in general and oceanography, in particular. The continental margins and the deep ocean basins are the two major aspects to be understood in this subject. This lesson is on the characteristics of continental margins.
Sedimentary basins are the depressions in the earth's crust where loose particles accumulate and finally lithified to form sedimentary rocks. Basins are particularly attractive to geoscientists from time immemorial due to the wealth hidden here in the form of oil, gas, coal etc. In this document you will find the types of basins, basin-fill types, methods of basin analysis and so on.
This is my presentation on the tectonic control of sediments.
It includes the effects of tectonics either direct or indirect on sediments and sedimentation.
Sedimentation along various plate boundaries.
Few examples as evidence from Pakistan (the Siwalik Group) and Argentina (Fiambala Basin)
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
A Strategic Approach: GenAI in EducationPeter Windle
Artificial Intelligence (AI) technologies such as Generative AI, Image Generators and Large Language Models have had a dramatic impact on teaching, learning and assessment over the past 18 months. The most immediate threat AI posed was to Academic Integrity with Higher Education Institutes (HEIs) focusing their efforts on combating the use of GenAI in assessment. Guidelines were developed for staff and students, policies put in place too. Innovative educators have forged paths in the use of Generative AI for teaching, learning and assessments leading to pockets of transformation springing up across HEIs, often with little or no top-down guidance, support or direction.
This Gasta posits a strategic approach to integrating AI into HEIs to prepare staff, students and the curriculum for an evolving world and workplace. We will highlight the advantages of working with these technologies beyond the realm of teaching, learning and assessment by considering prompt engineering skills, industry impact, curriculum changes, and the need for staff upskilling. In contrast, not engaging strategically with Generative AI poses risks, including falling behind peers, missed opportunities and failing to ensure our graduates remain employable. The rapid evolution of AI technologies necessitates a proactive and strategic approach if we are to remain relevant.
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.
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!
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How to Make a Field invisible in Odoo 17Celine George
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3. Continental Shelf
Submerged part of the continent
Slopes gently toward ocean basin
(<1°)
Composed of continental crust
Shelf ends at shelf break –
boundary between shelf and
steeper slope
4. Continental Slope
Boundary between continental
and oceanic crust
Steeply sloping compared to shelf
(5-25°)
Submarine canyons are major
features
Extends from shelf break to rise
6. Submarine Canyon
Turbidity Currents
Turbidites are layered and exhibit graded bedding (decrease in
sediment grain size from bottom to top)
Downslope movement of dense mixture of clay, silt, sand and water
Deposits are called turbidites
7. Continental Rise
At base of continental slope
Slope angle decreases
Caused by the accumulation of sediment
11. Continental Margin
Active
Convergent plate boundary
Trenches are boundaries
Tectonically active
Thin accumulation of
sediments
Narrow continental margin
12. Continental Margin
Passive vs. Active
Passive Margins
• Major rivers drain into ocean
• Sediment transported by
river builds out shelf
Active Margins
• Large rivers uncommon
• Irregular shelves
15. Ocean Basin Floor
Features
Seamounts and Guyots
Coral Reefs and Atolls
Ridges and Rises
Abyssal Plain
Trenches
16. Ocean Basin Floor
Covers about 30% of Earth’s surface
Contain abyssal plains, deep sea trenches, and seamounts
Begins at base of continental rise
Sedimentation: Passive and turbidity currents
17. Ocean Basin Floor
Abyssal Plain
Flat, deep ocean floor
Depth may be 2-3 miles or more
Thick sediment accumulation covers oceanic crust
18. Ocean Basin Floor
Deep Sea Trenches
Occur at subduction zones
where oceanic crust is
forced downward into
mantle
Associated with earthquakes
and volcanoes
Deepest is Mariana Trench
(11,020 m)
Longest is Peru-Chile trench
(5,900 km)
19. Ocean Basin Floor
Ridges and Rises
Contain central rift valleys
• 15-50 km wide
• 500-1,500 m deep
Offset by fractures
Underwater volcanic mountain chain
• Extends for 65,000 km
• 1,000 km wide
• 1,000-2,000 m high
Ridges = steep slopes
Rises = gentle slopes
20. Ocean Basin FloorOcean Basin Floor
Seamounts and GuyotsSeamounts and Guyots
Seamounts are underwater volcanoes formed along
ocean ridges or over hot spots
May be eroded flat on top and called Guyots
May emerge as an island
21. Ocean Basin Floor
Coral Reefs and Atolls
Volcanic islands (from seamount) form in warm latitudes
Fringing coral reefs form in shallow, sunlit waters
Dormant volcano subsides and flattens (becomes a guyot)
Actively-growing reef becomes a barrier reef and then an atoll
Editor's Notes
continental shelf lies at edge of continent; flat border of varying widths that slopes very gently toward ocean basin (part of continent; can be covered or uncovered by fluctuations in sea level); composed of continental crust; averages about 41 mi (10-300 km) with depths of 430 ft (130 m)
can have continental islands that are part of shelf
wide at passive margins
narrow at active margins, but width also depends on currents (rapid ones prevent sediment buildup) and sea level (narrow when sea level is low; broad when sea level is high)
continental shelf ends at the shelf break, where the slope abruptly gets steeper; usually occurs at 400 to 600 ft (100-200 m) but Antarctica, Greenland are exceptions because of their ice caps
continental slope is the exact edge of the continent
descends downward toward deep sea floor (3-5 km)
formed of sediments that reach the shelf break and slide down the slope
can also be composed of marine sediments scraped off a subducting plate at an active margin
steeper at an active margin than at a passive one, but still doesn&apos;t exceed an inclination of 25° (4° incline is average)
submarine canyons (can sometimes extend up, into, and across the continental shelf) are steep-sided and has a V-shaped cross section, with tributaries similar to those of river-cut canyons on land
carry sediments from shelf to sea floor -- is called down-slope transport of sediments; terminate in a fan-shaped wedge of sediment on deep sea floor
formed by turbidity currents which occur when turbulence mixes sediments into water and creates functional equivalent of a mud slide along the continental shelf and down the continental slope -- sediments are abrasive, so over time they cut into shelf&apos;s crust forming a canyon
continental rise is a gentle slope at the base of a steep continental slope
caused by the accumulation of sediment at a submarine canyon&apos;s base or at the base of the continental slope
descend 2-4 km to the abyssal plain (~4 km depth)
abyssal plain: flat plain extending seaward from the base of the continental slope
flatter than any plain on land; formed from sediments covering irregular topography of the seafloor
comprises 25% of earth&apos;s surface
The East Pacific Rise between the Pacific plate and the Nazca plate (where spreading rate is ~17 cm per year) causes a gentle sloping rise; in contrast, the slower spreading along the Mid-Atlantic Ridge (~5 cm per year) results in a steep slope characteristic of ridges; earthquake energy is closely related to the spreading rate and is higher at slower spreading centers
seamounts and guyots are volcanoes that arise originally at an oceanic ridge but then are carried away from the ridge by plate movement -- as they move, volcanic activity gradually decreases (the cracks in the earth&apos;s crust that serve as conduits for rising lava seal off)
however, while they are moving, there is still volcanic activity and they grow in height (seamounts)
the volcanoes can be active for 10-15 million years, but will eventually become dormant (few are active past 30 million years)
at this point the top will become flattened by wave action and will once again become submerged (guyots)
coral reefs -- origin proposed originally by Darwin before the theory of plate tectonics was formalized (called the subsistence theory of volcanic islands) -- several steps to this process:
volcanic island (from a seamount) forms in warm-water latitudes and a fringing coral reef forms in the shallow, sunlit waters adjacent to it
as the dormant volcano erodes due to the closing off of the cracks providing magma, the reef maintains its elevation near the surface because new corals build on the skeletons of old corals -- this new building produces a barrier reef where the actively growing reef is separated from the receding seamount by a well-developed lagoon
island flattens submerges (becomes a guyot) but reef continues to grow upward to produce an atoll with active reef growth confined to the outer edges (the interior of the atoll is a shallow lagoon)
Constructed primarily from skeletal remains and secretions of corals and certain algae
Confined largely to the warm, clear waters of the Pacific and Indian Oceans
Coral islands – a continuous ring of coral reef surrounding a central lagoon
Form on the flanks of a sinking volcanic island (hypothesis proposed by Charles Darwin)
Coral islands – a continuous ring of coral reef surrounding a central lagoon
Form on the flanks of a sinking volcanic island (hypothesis proposed by Charles Darwin)