Amundsen Plain refers to a geographical area located within the larger context of Antarctica. It is situated on the western side of the Antarctic Peninsula, specifically within the region called the Antarctic Sound, which lies between the Antarctic mainland and various islands, including the northern part of the Antarctic Peninsula. The plain is named after the Norwegian explorer Roald Amundsen, who was one of the first to reach the South Pole.
The Barents Basin is a major sedimentary basin located in the northern part of Europe, primarily beneath the Barents Sea. It is part of the larger Arctic region and is bordered by the Norwegian coast to the west, the Kola Peninsula to the southwest, and the Franz Josef Land archipelago to the north. The Barents Basin is notable for its geological and hydrocarbon potential.
Bowers Canyon is a geographical feature located in the state of Washington, specifically within the Gifford Pinchot National Forest. It is known for its scenic beauty, hiking trails, and outdoor recreational opportunities. The canyon typically features rugged terrain, lush forests, and waterways that attract visitors interested in hiking, camping, fishing, and photography.
The term "Cato Trough" refers to a specific geographical feature in Antarctica, specifically located in the southeastern part of the continent. It is a deep, glacially eroded valley or trough that is situated between the South Polar Plateau and the surrounding mountainous regions. The Cato Trough is characterized by significant ice coverage, with glaciers flowing into it from adjacent areas. Geological features like the Cato Trough contribute to our understanding of glaciation processes and the climatic history of Antarctica.
Dellwood Seamounts, also known as the Dellwood Seamounts, is a group of underwater volcanic mountains located in the Pacific Ocean. These seamounts are part of the larger tectonic and geological features found on the sea floor, formed by volcanic activity. They are situated to the east of the Hawaiian Islands and are part of the Hawaiian-Emperor seamount chain.
The East Shetland Basin is a geological formation located in the North Sea, off the northeastern coast of Scotland. It is part of the larger northern North Sea oil and gas province. The basin is characterized by a series of sedimentary deposits and is primarily known for its hydrocarbon resources, including oil and natural gas reserves. The East Shetland Basin has been a significant area of exploration and production for the oil and gas industry since the 1970s.
Ferrel Seamount is an underwater volcano located in the North Pacific Ocean. It is part of the Aleutian Arc, a volcanic island arc that is situated near the northern edge of the Pacific Plate. Ferrel Seamount is known for its steep underwater slopes and prominent peak, which rises significantly from the ocean floor. The seamount is primarily composed of volcanic rocks, and like many seamounts, it may host a variety of marine life due to the nutrient-rich waters that surround it.
The Gakkel Ridge Caldera is a volcanic structure located in the Arctic Ocean, specifically along the Gakkel Ridge, which is a mid-ocean ridge extending through the Arctic region. This caldera is of significant interest to geologists and volcanologists because it represents a unique environment where geological processes related to plate tectonics and volcanism occur beneath thick sea ice.
The Gotland Basin is a marine area located in the Baltic Sea, specifically to the east of Sweden and west of the Baltic island of Gotland. It is characterized by its relatively deep waters compared to surrounding areas, with depths that can reach up to approximately 250 meters (820 feet). The basin is significant for its geological features, marine ecosystems, and its role in regional hydrology.
The Mascarene Basin is a geological and oceanographic region located in the Indian Ocean, primarily situated between the islands of Mauritius and Réunion. It is named after the Mascarene Islands, which include these two islands as well as Rodrigues Island. The basin is characterized by its relatively shallow depths, with areas featuring a rich diversity of marine life and unique ecosystems.
Monaco Bank, also known as Monaco Volcano, is an underwater volcano located in the southwestern Pacific Ocean. It is a part of the "Vanuatu archipelago" and is situated near the island of Efate. This submarine volcano is known for its eruptive activity and contributes to the geological and volcanic features of the region. The volcano is closely monitored due to its potential to erupt and affect nearby islands and marine environments.
The Nordenskjöld Basin is a geological feature located in Antarctica, specifically in the eastern part of the continent within the broader context of the Antarctic Peninsula region. It is characterized by its sedimentary deposits and geological formations, which provide valuable information about the Earth's history, climate changes, and the geological evolution of Antarctica. The basin is named after the Swedish explorer Otto Nordenskjöld, who played a significant role in Antarctic exploration in the early 20th century.
Pennell Bank is a submerged bank located in the North Atlantic Ocean, specifically in the southeastern part of the Bermuda Triangle. It is situated approximately 34 miles northeast of the island of Bermuda. The bank is characterized by its shallow waters, which can pose a hazard to navigation for larger vessels. Pennell Bank is notable for being a historical reference point for maritime navigation and has been involved in various discussions regarding marine ecology and the unique ecosystems that may exist in such submerged areas.
Plantagenet Bank, also referred to as "The Plantagenet Bank," is a niche financial institution based in the UK. Established in 2021, it is primarily focused on serving the banking needs of small to medium-sized enterprises (SMEs), startups, and the agricultural sector. The bank offers various financial products, including business accounts, loans, and support tailored to the unique requirements of these business segments.
Quiroga Ridge is a geographical feature located in Antarctica, specifically on the continent's northeastern region. It is part of the larger Sentinel Range in the Ellsworth Mountains. The ridge is known for its rugged terrain and dramatic landscapes, typical of the Antarctic region. Named after the Argentine explorer and writer, Horacio Quiroga, Quiroga Ridge signifies the human connection to exploration and literature in one of the most remote areas of the world.
Rosenthal Seamount is an underwater volcanic feature located in the Pacific Ocean, specifically within the region of the northwestern Hawaiian Islands. It is part of the Hawaiian-Emperor seamount chain, which is a series of underwater mountains formed by volcanic activity associated with the movement of the Pacific tectonic plate over a hotspot in the Earth's mantle. Seamounts like Rosenthal are generally characterized by their significant height relative to the surrounding sea floor, and they can host diverse and unique ecosystems.
The South Shetland Trough is a significant geological feature located in the Southern Ocean, specifically surrounding the South Shetland Islands, which are situated north of the Antarctic Peninsula. This trough is a deep-sea trench that forms part of the complex bathymetry of the region, characterized by its significant depths and various geological formations.
Pinned article: Introduction to the OurBigBook Project
Welcome to the OurBigBook Project! Our goal is to create the perfect publishing platform for STEM subjects, and get university-level students to write the best free STEM tutorials ever.
Everyone is welcome to create an account and play with the site: ourbigbook.com/go/register. We belive that students themselves can write amazing tutorials, but teachers are welcome too. You can write about anything you want, it doesn't have to be STEM or even educational. Silly test content is very welcome and you won't be penalized in any way. Just keep it legal!
Intro to OurBigBook
. Source. We have two killer features:
- topics: topics group articles by different users with the same title, e.g. here is the topic for the "Fundamental Theorem of Calculus" ourbigbook.com/go/topic/fundamental-theorem-of-calculusArticles of different users are sorted by upvote within each article page. This feature is a bit like:
- a Wikipedia where each user can have their own version of each article
- a Q&A website like Stack Overflow, where multiple people can give their views on a given topic, and the best ones are sorted by upvote. Except you don't need to wait for someone to ask first, and any topic goes, no matter how narrow or broad
This feature makes it possible for readers to find better explanations of any topic created by other writers. And it allows writers to create an explanation in a place that readers might actually find it.Figure 1. Screenshot of the "Derivative" topic page. View it live at: ourbigbook.com/go/topic/derivativeVideo 2. OurBigBook Web topics demo. Source. - local editing: you can store all your personal knowledge base content locally in a plaintext markup format that can be edited locally and published either:This way you can be sure that even if OurBigBook.com were to go down one day (which we have no plans to do as it is quite cheap to host!), your content will still be perfectly readable as a static site.
- to OurBigBook.com to get awesome multi-user features like topics and likes
- as HTML files to a static website, which you can host yourself for free on many external providers like GitHub Pages, and remain in full control
Figure 3. Visual Studio Code extension installation.Figure 4. Visual Studio Code extension tree navigation.Figure 5. Web editor. You can also edit articles on the Web editor without installing anything locally.Video 3. Edit locally and publish demo. Source. This shows editing OurBigBook Markup and publishing it using the Visual Studio Code extension.Video 4. OurBigBook Visual Studio Code extension editing and navigation demo. Source. - Infinitely deep tables of contents:
All our software is open source and hosted at: github.com/ourbigbook/ourbigbook
Further documentation can be found at: docs.ourbigbook.com
Feel free to reach our to us for any help or suggestions: docs.ourbigbook.com/#contact





