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LATEST ARTICLES
Bihar Board 12th Result 2023: BSEB to Announce Intermediate Results Soon
The Bihar School Examination Board (BSEB) is gearing up to announce the much-awaited Class 12th results for 2023. Students across the state have been eagerly waiting for the release of their Intermediate scores, which are expected to be declared soon on the official website, biharboardonline.bihar.gov.in.
Various sources, including Live Hindustan, TV9 Hindi, Hindustan Times, and Jagran, have been providing live updates on the announcement, keeping students and their families informed of the latest developments. As students prepare to discover their scores, they are encouraged to keep an eye on these news sources for accurate and up-to-date information.
Once the results are officially released, students can access their scores by visiting the BSEB website at biharboardonline.bihar.gov.in. To check the results, they will need to enter their roll number and other relevant details as prompted. In addition, several alternative websites, such as sarkariresult.com, may also provide access to the Class 12th results.
The Bihar Board Class 12th exams were conducted in February, with thousands of students participating in the annual examinations. The board has since been working diligently to evaluate the answer sheets and compile the results. In previous years, the pass percentage and overall performance of students have seen steady improvement, and this year’s candidates hope to continue that trend.
As the BSEB readies itself to declare the Class 12th results, students across Bihar are encouraged to remain patient and stay informed via the provided news sources. The announcement of these results marks a significant milestone in their academic journey, and we wish all the students the best of luck in their future endeavors.
How Are Sedimentary Rocks Formed?
Sedimentary rocks are formed through the process of sedimentation, in which sediment is deposited in layers over time, and then lithified, or turned into rock, through the process of compaction and cementation. The process of sedimentation begins with the weathering and erosion of preexisting rocks, which breaks the rocks down into smaller fragments. These fragments, or sediment, can be transported by water, wind, ice, or gravity to a location where they are deposited.
Once the sediment is deposited, it can be compacted and cemented together by the weight of overlying layers, or by the precipitation of minerals from solution. The process of compaction involves the squeezing together of the sediment particles, which reduces the volume of the sediment and increases its density. The process of cementation involves the bonding of the sediment particles together through the precipitation of minerals, such as quartz or calcite, from solution.
The type of sedimentary rock that forms depends on the size and type of sediment that is deposited, as well as the conditions under which it is deposited. For example, sandstone is a clastic sedimentary rock that forms from the consolidation of sand-sized particles, while limestone is a chemical sedimentary rock that forms from the precipitation of calcite from solution.
Sedimentary rocks are often found in layers or strata, and these layers can be used to infer the relative ages
What is Sedimentary Rock and Types of sedimentary rocks?
Sedimentary rock is a type of rock that forms from the accumulation and consolidation of sediment, such as sand, clay, or mud. Sedimentary rocks are formed through the process of sedimentation, in which sediment is deposited in layers over time, and then lithified, or turned into rock, through the process of compaction and cementation.
There are several types of sedimentary rocks, including:
- Clastic sedimentary rocks: These rocks are made up of fragments of other rocks that have been broken down and transported by erosion and then deposited and lithified. Examples include sandstone, shale, and conglomerate.
- Chemical sedimentary rocks: These rocks are formed from the precipitation of minerals from solution. Examples include limestone, rock salt, and gypsum.
- Organic sedimentary rocks: These rocks are formed from the accumulation of organic matter, such as plant or animal remains. Examples include coal and some limestones.
- Biochemical sedimentary rocks: These rocks are formed through the chemical alteration of organic matter. Examples include chert and some limestones.
- Sedimentary rocks can be classified based on the size and type of sediment they contain. For example, sandstone is a clastic sedimentary rock that is composed of sand-sized particles, while shale is a clastic sedimentary rock that is composed of fine-grained, clay-sized particles.
- Sedimentary rocks often have distinctive features that can help geologists identify them and determine their origin. For example, sandstone often has visible layers or bedding planes, and conglomerate may contain rounded pebbles or cobbles.
- Sedimentary rocks can be further classified based on the type of cement that holds the sediment particles together. For example, sandstone can be classified as quartz sandstone if it is cemented with quartz, or as arkose if it is cemented with feldspar.
- Some sedimentary rocks, such as shale, can be transformed into metamorphic rocks through the process of metamorphism, in which the rock is subjected to high pressures and temperatures.
- Sedimentary rocks are formed at or near the Earth’s surface, and are often found in layers or strata. These layers can be used to infer the relative ages of the rocks, and to understand the geologic history of an area.
- Sedimentary rocks are important sources of information about past environments and the evolution of Earth’s surface. They can provide clues about the climate, vegetation, and wildlife that existed in a particular area in the past.
What are the different methods used to determine the relative ages of rocks and sedimentary layers?
Geologists use several methods to determine the relative ages of rocks and sedimentary layers. These methods are based on the principles of stratigraphy, which is the study of rock layers and the layering process. The methods include:
- The principle of superposition: In an undisturbed sequence of sedimentary rocks, the oldest layers are found at the bottom, with younger layers on top.
- The principle of original horizontality: Sedimentary layers are usually deposited in a horizontal or nearly horizontal position. If layers are tilted or folded, it may indicate tectonic activity.
- The principle of cross-cutting relationships: If one geologic feature cuts across another, it is younger than the feature it cuts. For example, a fault that cuts across a layer of sedimentary rock is younger than the rock it cuts through.
- The principle of inclusions: If one rock body contains pieces of another rock, it is younger than the rock it contains.
- Biostratigraphy: The use of fossils to determine the relative ages of rocks and sedimentary layers. Fossils can be used to establish the relative ages of rocks because different species of organisms lived at different times in Earth’s history.
- Stratigraphic correlation: The comparison of rock layers and sedimentary sequences in different areas to determine their relative ages and to understand the larger geologic history of an area.
- Stratigraphy and tectonics: The study of how tectonic processes, such as plate tectonics and mountain building, have shaped the stratigraphic record and influenced the evolution of Earth’s surface.
- Stratigraphy and paleoenvironmental reconstruction: The use of stratigraphy to understand past environments and the processes that shaped them.
- Stratigraphy and resource evaluation: The use of stratigraphy to understand the distribution of mineral and energy resources, and to evaluate their potential for extraction.
- Stratigraphy and geological hazards: The use of stratigraphy to understand geological hazards and their potential impacts on human activity.
- Geochronology and radiometric dating: The use of isotope ratios and radioactive decay to determine the absolute ages of rocks and sedimentary layers. This method can be used to establish the ages of rocks and sedimentary layers with greater precision than the relative dating methods mentioned above.
- Stratigraphic sequences: The sequence of sedimentary layers or strata that reflects a particular time period or geologic event. By studying the characteristics of the layers and the fossils they contain, geologists can infer the relative ages of the layers and the environments in which they were deposited.
What is stratigraphy and how is it used in geology?
Stratigraphy is the study of rock layers and the layering process, an important aspect of geology. It is used to understand the geologic history of an area, including the ages of the rocks, the environments in which they were formed, and the processes that shaped them. A stratigraphy is a powerful tool for reconstructing past environments and understanding the evolution of Earth and its surface features. It is used to understand the geologic history of an area, including the ages of the rocks, the environments in which they were formed, and the processes that shaped them. Stratigraphy is also used in searching for and evaluating mineral and energy resources and in studying geological hazards and their potential impacts on human activity.
In order to study stratigraphy, geologists rely on a number of principles and techniques, including:
- The principle of superposition: In an undisturbed sequence of sedimentary rocks, the oldest layers are found at the bottom, with younger layers on top.
- The principle of original horizontality: Sedimentary layers are usually deposited in a horizontal or nearly horizontal position. If layers are tilted or folded, it may indicate tectonic activity.
- The principle of cross-cutting relationships: If one geologic feature cuts across another, it is younger than the feature it cuts. For example, a fault that cuts across a layer of sedimentary rock is younger than the rock it cuts through.
- The principle of inclusions: If one rock body contains pieces of another rock, it is younger than the rock it has.
- Biostratigraphy: The use of fossils to determine the relative ages of rocks and sedimentary layers. Fossils can be used to establish the relative ages of rocks because different species of organisms lived at different times in Earth’s history.
- Geochronology and radiometric dating: The use of isotope ratios and radioactive decay to determine the absolute ages of rocks and sedimentary layers.
- Stratigraphic correlation: The comparison of rock layers and sedimentary sequences in different areas to determine their relative ages and to understand the larger geologic history of an area.
Top 20 Must-See Attractions and Activities in Tokyo
Tokyo has a rich history and a unique culture, and there are many things to see and do there. Here are a few suggestions for things to do in Tokyo:
- Visit the Tokyo Skytree: This iconic tower is the tallest structure in Japan, and it offers panoramic views of the city from its observation decks.
- Explore the gardens and temples of the Asakusa district: This historic neighborhood is home to the Sensoji Temple and several beautiful gardens and traditional streets.
- Visit the Tokyo Metropolitan Government Building: This building offers free observation decks on the 45th floor, which provide stunning views of the city.
- Check out the Tokyo National Museum: This museum houses a vast collection of Japanese art and cultural artifacts, including ancient ceramics, paintings, and samurai armor.
- Take a stroll through the bustling streets of Shibuya: This popular neighborhood is known for its shopping, dining, and nightlife, and it’s a great place to people-watch.
- Visit the Meiji Shrine: This beautiful shrine is located in a peaceful forest in the city’s center and is a popular spot for visitors to experience traditional Japanese culture.
- Try some local food: Tokyo is known for its incredible food scene, and there are many delicious dishes to try, including sushi, ramen, and tempura.
- Visit the Tokyo Disney Resort: This popular theme park is located just outside the city and is a great place to have fun with the whole family.
- Take a trip to the Edo-Tokyo Museum: This museum offers a fascinating look at the history of Tokyo, from its founding as Edo in the 17th century to its modern-day status as a global city.
- Go shopping in Ginza: This upscale shopping district is home to many luxury brands and great places to find souvenirs or indulge in some retail therapy.
- Visit the Tokyo Tower: This iconic structure was once the tallest building in Japan and offered great views of the city from its observation decks.
- Explore the Tokyo National Science Museum: This museum is a great place to learn about the latest scientific discoveries and technology.
- Visit the Tokyo Metropolitan Art Museum: This museum features a variety of art exhibits, including contemporary and traditional Japanese art.
- Check out the Tokyo Metropolitan Teien Art Museum: This museum is housed in a beautiful Art Deco building and features a variety of art exhibits and events.
- Take a stroll through the Hamarikyu Onshi Teien: This beautiful garden is located on the edge of Tokyo Bay and features a traditional Japanese garden and a teahouse.
- Visit the Ueno Zoo: This popular zoo is home to various animals, including pandas, elephants, and gorillas.
- Take a trip to Odaiba: This man-made island is home to several popular attractions, including the Oedo Onsen Monogatari hot springs, the Tokyo Joypolis theme park, and the Miraikan science museum.
- Explore the Tsukiji Fish Market: This bustling market is the world’s largest wholesale fish and seafood market and is a great place to try fresh sushi and other seafood dishes.
- Visit the Yoyogi Park: This large park is a popular spot for picnics and outdoor activities, and it’s also home to the Meiji Jingu Shrine.
- Take a tour of the Suntory Whisky Distillery: This distillery is located in the heart of Tokyo and offers tours and tastings of its various whisky brands.
Netflix’s Cheaper Plan: All the Movies and Shows You Can’t Watch
On Thursday, Netflix introduced a new plan that is both more affordable and includes advertisements. These advertisements bring with them some restrictions: A significant number of television series and motion pictures are unavailable due to licencing limitations. You can search via the Netflix platform to find anything that has a lock mark on it. However, Netflix has not released a comprehensive list of episodes and movies that are not currently available. These movies and TV shows are not available to stream on the Netflix Basic With Ads package.
The following is a list of notable television shows and motion pictures that are not currently available on Netflix’s Basic plan with advertisements:
Unavailable TV shows
- Arrested Development
- Breaking Bad
- Grey’s Anatomy
- How to Get Away With Murder
- The Crown
- Cobra Kai
- House of Cards
- Peaky Blinders
- New Girl
- The Magicians
- The Last Kingdom
- The Sinner
- Good Girls
- The Good Place
- Friday Night Lights
Unavailable movies
- Skyfall
- 28 Days
- The Imitation Game
- The Bad Guys
Google Chat adds phishing warnings
According to an announcement made by Google on Thursday, Google Chat has replaced Google Hangouts and will now display banners warning you against the possibility of phishing and malware attacks coming from personal accounts. The most recent development in Google’s ongoing fight against phishing is a change that has been made to Google Chat.
During the 2022 I/O developer conference, Google discussed several security measures it has implemented to enhance user safety. These security measures include warnings against potential security issues as well as recommendations to fix them. In addition, Google detailed additional plans for additional security measures, including the expansion of their two-step verification system, ad customization, and increased data security.
The new warning banners that were introduced by Google initially appeared in Gmail on Workspace accounts. Their purpose was to draw attention to attempts to trick someone into clicking on a link that could be used to spread malware, phishing attacks, or ransomware. At the end of April, Google extended the banners to Google Docs, warning users against suspected malicious files in several Google Workspace apps (Docs, Sheets, Slides, and Drawing) regardless of where the link was opened from. This was done in conjunction with the expansion of the banners to Google Drive.
This new feature will be rolled out over the next couple of weeks, and it will be available for use with personal Google accounts as well as with accounts belonging to customers of Google Workspace.
Devil’s Lake State Park in Wisconsin has 10 of the best hiking trails.
Devil’s Lake State Park is a must-visit if you want to experience some of Wisconsin’s most breathtaking natural scenery and top hiking routes.
Since there are no mountains in America’s Dairyland, hiking at high altitudes is also not really a thing there. Wisconsin makes up for its lack of height, however, with unspoiled hardwood forests, miles of lakeshore, and unusual rock formations, all of which are located within the boundaries of Devil’s Lake State Park.
In fact, Wisconsin’s most visited state park is Devil’s Lake because of how stunning it is. It’s all due to the hiking routes that ascend 500-foot quartzite bluffs and the autumn’s vibrant foliage. However, there are more worthwhile activities here besides hiking! The park’s numerous picnic spaces, sandy lakefront, and contemporary campgrounds are all available to visitors.
Even the most experienced hiker will be enthralled by these outstanding hiking routes in Devils Lake State Park, which rank among the best in the state.
East Bluff Loop, first
Why you ought to go A well-liked hiking route that offers expansive lake vistas and traverses the eastside bluffs. The most well-liked hike in Devil’s Lake is the East Bluff Loop, and for good reason. With the exception of one section with a steep ascent, the trail is not especially challenging. However, it just takes a quarter of a mile to reach the top of the bluff. But after wiping your brow at the summit, you’ll be rewarded with stunning views of the surroundings. This route crosses paths with other well-liked hikes in the park as it follows the lake’s east side bluff. As you finish the loop, keep an eye out for Elephant Cave and Elephant Rock.West Bluff Trail 2.
Why you ought to go a path leading to the park’s highest point along the top of the western bluffs. Visit the West Bluff Trail to see the lake from a new angle. Starting the loop on the north or south side of the lake gives you a choice of two distinct experiences. Stone stairs must be climbed on the north end, while a steep climb must be climbed on the south end. There are a lot of undulating ups and downs on the West Bluff Trail, which could be difficult for some. Aside from the breathtaking vista, the highlight of this path is the chance to see the distinctive rock formations at Prospect Point and Cleopatra’s Needle in the park.3. West Bluff to Devil’s Lake Loop
Why you ought to go Hikers can traverse a sizable loop that circles Devil’s Lake’s shoreline. The lake is displayed in all its splendour from the Devil’s Lake via West Bluff Trail. What more could you want for when it has enormous boulders, steep bluffs, and lake views? There are numerous challenging climbs along the way because this path leads hikers up and over the cliffs on both sides. However, those that complete the entire loop are rewarded with panoramic views of the surroundings. The trailhead is close to a section of beach where you can cool yourself before or after starting your hike. It does run alongside a few other hiking paths because it is the park’s largest loop. Along the way, you pass notable sites including the Balanced Rock.Devil’s Doorway Trail, No. 4
Why you ought to go Another renowned rock feature in the park is reached after an adventurous trial. The Devil’s Doorway Trail, so named because it descends to a little arch made of a jumble of boulders from the East Bluff, is a brief loop. Less than a quarter-mile must be hiked to get reach the doorway from the East Bluff. With a clear view of the tranquil lake waters behind it, Devil’s Doorway is wonderfully framed by trees. This walk traverses small rock ledges and takes many people about an hour to complete, therefore care should be exercised. Since the Devil’s Doorway Trail isn’t well marked, many hikers advise taking the CCC trail markers on the way down.Balanced Rock Trail 5.
Why you ought to go There is a well-known trail that leads to Devil’s Lake’s most famous view. The East Bluff is reached at the top of the Balanced Rock Trail, which is a steep and difficult hike. Technically an out and back, the track is actually relatively short. The East Cliff Trail, a comparatively flat walk across the bluff top, is where most hikers carry on. Before you reach the summit, you can enjoy views of the Balanced Rock, which is a lovely little diversion from the difficult ascent. This is one of the park’s busiest routes, and the summer and fall may be very crowded there. A sizable boulder that fell and landed perfectly balanced on a pedestal facing the lake is known as Balanced Rock in the park.6. Trail to Devil’s Lake Grottos
Why you ought to go An easy stroll takes you through the forest to the south bank of the lake. The Devil’s Lake Grottos Trail is a tranquil hiking path that gives visitors access to many other amazing park locations. The Grottos Trail itself is a broad gravel trail that runs parallel to the East Bluff. The path begins at the lake and finishes at the CCC parking lot, and it is primarily shaded by the nearby forests. Additionally, it links to the Potholes Trail, which is worthwhile detouring to view because of the historic potholes that were worn by rushing water. The short CCC route has steep stone steps that climb to the top of the bluff and is also accessible via Grottos. Hikers can even stray to the renowned Balanced Rock if they’re interested.7. Trail of Tumbled Rock
Why you ought to go A one-hour hike along a paved, open trail that follows the shore of the lake. For hikers looking for a leisurely stroll or for families, the Tumbled Rock Trail is ideal. Throughout your trek, you can awe at the close-up views of the lake and bluff. The walk is so near to the lake that you may, if you’d like, dip your feet in or take a little swim. Additionally, as the name suggests, this trail climbs the side of the cliffs and goes by big rocks that are strewn everywhere around the lake. Since there are so many rocks and stones, these are essentially what set this trial apart. If you have a dog that can’t manage the steep hills, this trail is also fantastic for you, just keep your pet on a leash.Uplands Trail 8.
Why you should go: The area around the lake has a less-traveled hiking track through farmland and forests. The Uplands Trail is a special approach to see the scenery near and distant from Devil’s Lake’s actual shoreline. This loop offers a longer hiking experience than many other trails inside the state park area because it is approximately four miles long. The main features of this trail are thickets of hardwoods and sprawling meadows. There are, however, a few vantage spots from where you may see the Wisconsin River. Depending on the weather, mountain riding is allowed on the Uplands Trail. For even more hiking enjoyment, check out the adjacent Steinke Basin Loop.9. Devil’s Lake to Parfrey’s Glen on the Ice Age Trail
Why you ought to go a lengthy stretch of the Ice Age Trail that leads to a gorge with a waterfall that is 100 feet tall. The Ice Age Trail connects Devil’s Lake and Parfrey’s Glen for those looking for a lengthier hike. The approximately 1,200-mile national Ice Age Trail in Wisconsin is a thrilling path that circles the state. It displays the stunning topography that glaciers carved out when they once writhed across the state. The Devil’s Lake and Sauk Point sections of the national trail are both followed on this specific trek. You’ll come across several rises, patches of woods, and a county highway crossing on your trip. Either a point-to-point hike or a circle that covers almost 17 miles can be completed. At the conclusion of your lengthy journey, you will traverse Parfrey’s Glen, a rocky and mossy ravine. The trail of this broad valley is surrounded by enormous boulders, sandstone cliff walls, and a tranquil stream.10. Trail to Pewit’s Nest
Why you should go: There is a renowned, steep gorge on a short but delightful trip outside of the state park. The magnificent Pewit’s Nest Trail is located less than ten minutes’ drive from Devil’s Lake. Despite requiring little effort or stamina, this trail is well worth the drive. A clearly indicated dirt road through the woods leads to the amazing sandstone formations from the parking lot. The gorge is roughly 40 feet deep, with a flowing stream, many cascades, and pools of water. The ravine may be seen in just 20 minutes, but because of its close proximity to Devil’s Lake, it makes a great side trip.The Lost Creek Wilderness in Colorado has five fantastic hikes.
The Lost Creek Wilderness provides an outstanding setting for a day trek or backpacking excursion, with its spectacular granite formations, huge aspen woods, and above-treeline views.
The Platte River, Kenosha, and Tarryall Mountains, which are located in the 119,790-acre wilderness, contain a broad diversity of landscapes with elevations ranging from 8,000 feet to 12,400 feet. Within the 105-mile-long Lost Creek Wilderness (LCW), there are routes that lead through ponderosa, bristlecone, lodgepole pine, aspen, spruce, and fir woods and up to alpine tundra. Seeing the distinctive red granite domes and arches and having the ability to see animals including black bears, bighorn sheep, deer, elk, and bobcats are both attractions.
Many of the pathways are far-flung and lengthy in the large wilderness area. However, this is one wilderness region that will reward hikers who are willing to put in miles, whether you’re planning a lengthy day trek or a backpacking trip with a few overnight breaks. You may take shorter, easier out-and-back hikes from the numerous trailheads that reach Lost Creek. Be ready for strenuous days with high mileage and a lot of standing around if you really want to explore Lost Creek. The benefits are definitely worth the work.
Preparation is key. Bring plenty of water because there are lengthy sections without access to water, especially in the summer and fall, and many of the streams are seasonal. Even though there may not be any snow at lower levels in the spring, as you ascend into the mountains, you should expect to encounter snowpack until the end of May or the beginning of June. Day hikes and backpacking trips require wilderness permits, which are available for free at the wilderness boundary. Bailey, Deckers, Fairplay, and Lake George are the closest towns.