First Apache Server, Webpage Images Missing - html
I just built my first AWS Apache Server and uploaded my website from my school project. The site works in Dreamweaver. However on my Apache server only some of the images appear. They all have the same path and are contained in the same folder /var/www/html/images. Some appear as intended, others are a broken link. Any ideas why it's not working? To get css to load I had to move my css folder. With the images some work fine while others do not. They are roughly the same size files. This is the code for one of the non working images:
<img src="../images/heart_stone2.JPG" alt="Desert Jasper" class="list_photo">
Here is the whole page:
<!doctype html>
<html lang="en">
<head>
<meta charset="utf-8">
<link rel="stylesheet" type="text/css" href="../css/styles.css">
<!-- favicon code -->
<link rel="apple-touch-icon" sizes="180x180" href="../images/apple-touch-icon.png">
<link rel="icon" type="image/png" sizes="32x32" href="../images/favicon-32x32.png">
<link rel="icon" type="image/png" sizes="16x16" href="../images/favicon-16x16.png">
<link rel="manifest" href="../images/site.webmanifest">
<meta name="msapplication-TileColor" content="#da532c">
<meta name="theme-color" content="#ffffff">
<title>Rock list</title>
</head>
<body>
<h1>List of Rocks and Minerals</h1>
<figure>
<figcaption>Description of Jasper</figcaption>
<div class="bottom_mar"><img src="../images/heart_stone2.JPG" alt="Desert Jasper" class="list_photo"><p>Jasper is an opaque rock of virtually any color stemming from the mineral content of the original sediments or ash. Patterns arise during the consolidation process forming flow and depositional patterns in the original silica rich sediment or volcanic ash. Hydrothermal circulation is generally thought to be required in the formation of jasper.</p><p> Jasper can be modified by the diffusion of minerals along discontinuities providing the appearance of vegetative growth, i.e., dendritic. The original materials are often fractured and/or distorted, after deposition, into diverse patterns, which are later filled in with other colorful minerals. Weathering, with time, will create intensely colored superficial rinds.</p><p> The classification and naming of jasper varieties presents a challenge. Terms attributed to various well-defined materials includes the geographic locality where it is found, sometimes quite restricted such as "Bruneau" (a canyon) and "Lahontan" (a lake), rivers and even individual mountains; many are fanciful, such as "forest fire" or "rainbow", while others are descriptive, such as "autumn" or "porcelain". A few are designated by the place of origin such as a brown Egyptian or red African.</p></div>
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<figcaption>Description of Amethyst</figcaption>
<div class="bottom_mar"><img src="../images/amethyst2.jpg" alt="Uruguayan Amethyst" class="list_photo"><p>Amethyst was used as a gemstone by the ancient Egyptians and was largely employed in antiquity for intaglio engraved gems.</p><p>The Greeks believed amethyst gems could prevent intoxication, while medieval European soldiers wore amethyst amulets as protection in battle in the belief that amethysts heal people and keep them cool-headed. Beads of amethyst were found in Anglo-Saxon graves in England. Anglican bishops wear an episcopal ring often set with an amethyst, an allusion to the description of the Apostles as "not drunk" at Pentecost in Acts 2:15.</p><p>A large geode, or "amethyst-grotto", from near Santa Cruz in southern Brazil was presented at a 1902 exhibition in Düsseldorf, Germany.</p><p>In the 19th century, the color of amethyst was attributed to the presence of manganese. However, since it can be greatly altered and even discharged by heat, the color was believed by some authorities to be from an organic source. Ferric thiocyanate has been suggested, and sulfur was said to have been detected in the mineral.</p></div>
<div class="clear"></div>
<figcaption>Description of Siva Lingams</figcaption>
<div class="bottom_mar"><img src="../images/siva_lingams2.jpg" alt="Siva Lingams" class="list_photo"><p>All traditional lingams come from only one place in the entire world, the Narmada River in India, at Onkar, Mandhata, which is one of the country’s seven sacred holy sites. In this sacred place, lingams wash up on the banks of the river or are carefully brought up from the riverbed.</p><p>India has a long, dry period, and it is at this time, when the river is at its lowest, that the nearby residents go out to the banks of the Narmada and gently pull the stones from their resting places. The lingams are then polished by hand, using methods in accordance with Vedic tradition. Many believe that the lingams are already sacred when they are pulled from the river, but also that the energy given to each lingam during polishing makes it extra special.</p></div>
<div class="clear"></div>
<figcaption>Description of Desert Rose</figcaption>
<div class="bottom_mar"><img src="../images/desert_roses2.jpg" alt="Desert Roses" class="list_photo"><p>Desert rose is the colloquial name given to rose-like formations of crystal clusters of gypsum or baryte which include abundant sand grains. The 'petals' are crystals flattened on the c crystallographic axis, fanning open in radiating flattened crystal clusters.</p><p>The rosette crystal habit tends to occur when the crystals form in arid sandy conditions, such as the evaporation of a shallow salt basin. The crystals form a circular array of flat plates, giving the rock a shape similar to a rose blossom. Gypsum roses usually have better defined, sharper edges than baryte roses. Celestine and other bladed evaporite minerals may also form rosette clusters. They can appear either as a single rose-like bloom or as clusters of blooms, with most sizes ranging from pea sized to 4 inches (10 cm) in diameter.</p><p>The ambient sand that is incorporated into the crystal structure, or otherwise encrusts the crystals, varies with the local environment. If iron oxides are present, the rosettes take on a rusty tone.</p><p>The desert rose may also be known by the names: sand rose, rose rock, selenite rose, gypsum rose and baryte (barite) rose.</p><p>Rose rocks are found in Tunisia, Libya, Morocco, Algeria, Jordan, Saudi Arabia, Qatar, Egypt, the United Arab Emirates, Spain (Fuerteventura, Canary Islands; Canet de Mar, Catalonia; La Almarcha, Cuenca), Mongolia (Gobi), Germany (Rockenberg), the United States (central Oklahoma; Cochise County, Arizona; Texas), Mexico (Ciudad Juárez, Chihuahua), Australia, South Africa and Namibia.</p></div>
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<figcaption>Description of Aragonite</figcaption>
<div class="bottom_mar"><img src="../images/aragonite2.jpg" alt="Aragonite" class="list_photo"><p>The type location for aragonite is Molina de Aragón in the Province of Guadalajara in Castilla-La Mancha, Spain, for which it was named in 1797. The mineral is not (as often assumed) named for the region of Aragon: Molina de Aragón is located in the historic region of Castile, albeit only 25 kilometers away from the border with Aragon. Aragonite is found in this locality as cyclic twins inside gypsum and marls of the Keuper facies of Triassic.[4] This type of aragonite deposits are very common in Spain, and there are also some in France and Morocco.</p><p>An aragonite cave, the Ochtinská Aragonite Cave, is situated in Slovakia. In the US, aragonite in the form of stalactites and "cave flowers" (anthodite) is known from Carlsbad Caverns and other caves. Massive deposits of oolitic aragonite sand are found on the seabed in the Bahamas.</p><p>Aragonite is the high pressure polymorph of calcium carbonate. As such, it occurs in high pressure metamorphic rocks such as those formed at subduction zones.</p></div>
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<figcaption>Description of Apophyllite</figcaption>
<div class="bottom_mar"><img src="../images/aphopholite2.jpg" alt="Aphopholite" class="list_photo"><p>The name apophyllite refers to a specific group of phyllosilicates, a class of minerals. Originally, the group name referred to a specific mineral, but was redefined in 1978 to stand for a class of minerals of similar chemical makeup that comprise a solid solution series, and includes the members fluorapophyllite-(K), fluorapophyllite-(Na), hydroxyapophyllite-(K). The name apophyllite is derived from the Greek ἀποφυλλίζω apophylliso, meaning "it flakes off", a reference to this class's tendency to flake apart when heated, due to water loss. These minerals are typically found as secondary minerals in vesicles in basalt or other volcanic rocks. A recent change (2008) in the nomenclature system used for this group was approved by the International Mineralogical Association, removing the prefixes from the species names and using suffixes to designate the species. A subsequent nomenclature change approved by the International Mineralogical Association in 2013 renamed the minerals to include both suffixes and prefixes, as shown above.</p><p>Though relatively unfamiliar to the general public, apophyllites are fairly prevalent around the world, with specimens coming from some of the world's most well-known mineral localities. These localities include: Jalgaon, India; the Harz Mountains of Germany, Mont Saint-Hilaire in Canada, and Kongsberg, Norway, with other locations in Scotland, Ireland, Brazil, Japan, and throughout the United States.</p></div>
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<figcaption>Description of Calcite</figcaption>
<div class="bottom_mar"><img src="../images/calcite2.jpg" alt="Orange Banded Calcite" class="list_photo"><p>Ancient Egyptians carved many items out of calcite, relating it to their goddess Bast, whose name contributed to the term alabaster because of the close association. Many other cultures have used the material for similar carved objects and applications.</p><p>High-grade optical calcite was used in World War II for gun sights, specifically in bomb sights and anti-aircraft weaponry.[13] Also, experiments have been conducted to use calcite for a cloak of invisibility.</p><p>Calcite is a common constituent of sedimentary rocks, limestone in particular, much of which is formed from the shells of dead marine organisms. Approximately 10% of sedimentary rock is limestone. It is the primary mineral in metamorphic marble. It also occurs in deposits from hot springs as a vein mineral; in caverns as stalactites and stalagmites; and in volcanic or mantle-derived rocks such as carbonatites, kimberlites, or rarely in peridotites.</p><p>Calcite is often the primary constituent of the shells of marine organisms, e.g., plankton (such as coccoliths and planktic foraminifera), the hard parts of red algae, some sponges, brachiopods, echinoderms, some serpulids, most bryozoa, and parts of the shells of some bivalves (such as oysters and rudists). Calcite is found in spectacular form in the Snowy River Cave of New Mexico as mentioned above, where microorganisms are credited with natural formations. Trilobites, which became extinct a quarter billion years ago, had unique compound eyes that used clear calcite crystals to form the lenses.</p><p>The largest documented single crystal of calcite originated from Iceland, measured 7×7×2 m and 6×6×3 m and weighed about 250 tons.</p></div>
<div class="clear"></div>
<figcaption>Description of Spirit Quartz</figcaption>
<div class="bottom_mar"><img src="../images/spirit_quartz2.jpg" alt="Spirit Quartz" class="list_photo"><p>Spirit Quartz is an unusual member of the Quartz family - a community within a stone. Its core, a larger, candle-shaped crystal with a faceted termination point, is encrusted with hundreds of smaller crystal termination points. Also referred to as Cactus Quartz or Porcupine Quartz, it is found only in the Magaliesberg Mountain region of South Africa, first appearing around 2001. Most Spirit Quartz is Amethyst, though Citrine, Smokey, and White Quartz are also mined.</p><p>The word "quartz" is derived from the German word "Quarz", which had the same form in the first half of the 14th century in Middle High German in East Central German[8] and which came from the Polish dialect term kwardy, which corresponds to the Czech term tvrdý ("hard").</p><p>The Ancient Greeks referred to quartz as κρύσταλλος (krustallos) derived from the Ancient Greek κρύος (kruos) meaning "icy cold", because some philosophers (including Theophrastus) apparently believed the mineral to be a form of supercooled ice.[10] Today, the term rock crystal is sometimes used as an alternative name for the purest form of quartz.</p></div>
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<figcaption>Description of Moldavite</figcaption>
<div class="bottom_mar"><img src="../images/moldavite2.jpg" alt="Moldavite" class="list_photo"><p>Moldavite is a forest green, olive green or blue greenish vitreous silica projectile rock formed by a meteorite impact probably in southern Germany (Nördlinger Ries Crater)[3] that occurred about 15 million years ago. It is a type of tektite.</p><p>Moldavite was introduced to the scientific public for the first time in 1786 as "chrysolites" from Týn nad Vltavou in a lecture by Josef Mayer of Prague University, read at a meeting of the Bohemian Scientific Society (Mayer 1788). Zippe (1836) first used the term "Moldavite", derived from the Moldau (Vltava) river in Bohemia (the Czech Republic), from where the first described pieces came.</p><p>In 1900, F. E. Suess pointed out that the gravel-size moldavites exhibited curious pittings and wrinkles on the surface, which could not be due to the action of water, but resembled the characteristic markings on many meteorites. He attributed the material to a cosmic origin and regarded moldavites as a special type of meteorite for which he proposed the name of tektite. Because of their difficult fusibility, extremely low water content, and chemical composition, the current consensus among earth scientists is that moldavites were formed about 14.7 million years ago during the impact of a giant meteorite in the present-day Nördlinger Ries crater. Splatters of material that was melted by the impact cooled while they were actually airborne and most fell in Bohemia. Currently, moldavites have been found in an area that includes southern Bohemia, western Moravia, the Cheb Basin (northwest Bohemia), Lusatia (Germany), and Waldviertel (Austria). Isotope analysis of samples of moldavites have shown a beryllium-10 isotope composition similar to the composition of Australasian tektites (australites) and Ivory Coast tektites (ivorites).</p></div>
</figure>
<!-- links to local webpages -->
<nav>
<ul>
<li>Home Page</li>
<li>Rock List</li>
<li>Rock Images</li>
<li>Comments</li>
<li>Links</li>
<li>Email Me</li>
</ul>
</nav>
</body>
</html>
I found that the file extension on some of the pictures was capitalized. These pictures wouldn't load until I changed .JPG to .jpg.
Related
image not sticking at the bottom of the display with row and col class
My output is - as you can see, i have two rows, row left has the heading with select your hero moment text and carousel and row right has an image of a player. currently the player is floating in that row. I want to show the image sticked at the bottom of my display in that row. My html- <img src="images/CV.png" width="100%" style="position: -webkit-sticky; position:sticky; bottom:0;" id="my" alt="" > </div> as you can see i have tried the sticky position solution but didnt work for me.
Please try the below code. Kindly change the width and height based on your need.
#my{
position: fixed;
left: 0;
bottom: 0;
width: 100px;
height:100px;
}
<div>
<p>
"Aeroplane" redirects here. For other uses, see Airplane (disambiguation) and Aeroplane (disambiguation).
North American P-51 Mustang, a World War II fighter aircraft
The first flight of an airplane, the Wright Flyer on December 17, 1903
An All Nippon Airways Boeing 777-300 taking off from New York JFK Airport
An airplane or aeroplane (informally plane) is a powered, fixed-wing aircraft that is propelled forward by thrust from a jet engine, propeller or rocket engine. Airplanes come in a variety of sizes, shapes, and wing configurations. The broad spectrum of uses for airplanes includes recreation, transportation of goods and people, military, and research. Worldwide, commercial aviation transports more than four billion passengers annually on airliners[1] and transports more than 200 billion tonne-kilometers[2] of cargo annually, which is less than 1% of the world's cargo movement.[3] Most airplanes are flown by a pilot on board the aircraft, but some are designed to be remotely or computer-controlled such as drones.
The Wright brothers invented and flew the first airplane in 1903, recognized as "the first sustained and controlled heavier-than-air powered flight".[4] They built on the works of George Cayley dating from 1799, when he set forth the concept of the modern airplane (and later built and flew models and successful passenger-carrying gliders).[5] Between 1867 and 1896, the German pioneer of human aviation Otto Lilienthal also studied heavier-than-air flight. Following its limited use in World War I, aircraft technology continued to develop. Airplanes had a presence in all the major battles of World War II. The first jet aircraft was the German Heinkel He 178 in 1939. The first jet airliner, the de Havilland Comet, was introduced in 1952. The Boeing 707, the first widely successful commercial jet, was in commercial service for more than 50 years, from 1958 to at least 2013.
</p>
<img src="https://homepages.cae.wisc.edu/~ece533/images/airplane.png" width="100%" id="my" alt="" >
</div>
How to keep HTML lines under 80 characters?
I've been told to keep HTML lines under 80 characters. I'm using Atom, and there is displayed a line to remind it. I've found a lot of discussions about it but no example at all. For example, I have this line: <p> Born and raised in Valencia (Spain), graduated and married in Seville (Spain) and now I'm working and growing my own very family in Vienna (Austria). </p> and if I split it I get this: <p> Born and raised in Valencia (Spain), graduated and married in Seville (Spa in) and now I'm working and growing my own very family in Vienna (Austria) . </p> But when I look it on the browser there's a space between some words: Born and raised in Valencia (Spain), graduated and married in Seville (Spa_in) and now I'm working and growing my own very family in Vienna (Austria)_. (I typed underscores to point the generated spaces) How can I avoid this? And when it comes to code: How to split tags, attributes, links, etc.? For example: <link rel="apple-touch-icon image_src" href="https://cdn.sstatic.net/Sites/stackoverflow/img/apple-touch-icon.png?v=c78bd457575a"> or this <meta name="twitter:title" property="og:title" itemprop="title name" content="Ask a Question" /> Does anyone know any resource to consult? By the way, for the moment I'm just coding in HTML and not using JS at all, and I need to keep it like this if it's possible.
Split it close to 80 symbols. <p> Born and raised in Valencia (Spain), graduated and married in Seville (Spain) and now I'm working and growing my own very family in Vienna (Austria). </p> For tag splitting - split on every attribute: <link rel="apple-touch-icon image_src" href="https://cdn.sstatic.net/Sites/stackoverflow/img/apple-touch-icon.png?v=c78bd457575a" > Please note that it's sometimes better to exceed line limit to increase readability.
Just do it this way; you said under 80 so you don't need always 80. <p> Born and raised in Valencia (Spain), graduated and married in Seville (Spain) and now I'm working and growing my own very family in Vienna (Austria). </p> Other example with multiline property (you have to use tabs not spaced for the URL to work), but I recommend not to use this (like Justinas already mentioned in the comments), because it can lead to problems, sometimes it's better to adopt the rules: <img src="https://cdn.sstatic.net/Sites/stackoverflow/ img/apple-touch-icon.png?v=c78bd457575a">
How can I make my website not drag on mobile devices?
I keep running into a problem while building websites - on mobile devices, if you drag with your finger, the whole site moves around, moving partially outside the screen or wherever you drag it. I find this to be unprofessional and really ugly. Other websites I visit seem to have solved this problem but I have not been able to figure it out by looking at their source code. Any thoughts? Thanks in advance.
Probably <body draggable="false" ondragstart="return false"> See snippet for an example using a div container <div draggable="false" ondragstart="return false"> Robert Wertheimer Frucht (later known as Roberto Frucht) (9 August 1906 – 26 June 1997)[1][2] was a German-Chilean mathematician; his research specialty was graph theory and the symmetries of graphs. The Frucht graph. In 1908, Frucht's family moved from Brünn, Austria-Hungary (now in the Czech Republic), where he was born, to Berlin.[2] Frucht entered the University of Berlin in 1924 with an interest in differential geometry, but switched to group theory under the influence of his doctoral advisor, Issai Schur; he received his Ph.D. in 1931.[3][4] Unable to find academic employment in Germany due to his Jewish descent, he became an actuary in Trieste, but left Italy in 1938 because of the racial laws that came into effect at that time.[3][5] He moved to Argentina, where relatives of his wife lived, and attempted to move from there to the United States, but his employment outside academia prevented him from obtaining the necessary visa.[2][5] At the same time Robert Breusch, another German mathematician who had been working in Chile for three years but was leaving for the U.S., invited Frucht to fill his position at Federico Santa María Technical University in Valparaiso, Chile, where Frucht found an academic home beginning in 1939.[1][2][6] At Santa María, Frucht became dean of the faculty of mathematics and physics from 1948 to 1968, and retired to become an emeritus professor in 1970.[2] Frucht is known for Frucht's theorem, the result that every group can be realized as the group of symmetries of an undirected graph,[7][8] and for the Frucht graph, one of the two smallest cubic graphs without any nontrivial symmetries. LCF notation, a method for describing cubic Hamiltonian graphs, was named for the initials of Joshua Lederberg, H. S. M. Coxeter, and Frucht, its key developers.[9] Frucht was elected to the Chilean Academy of Sciences as a corresponding member in 1979.[2] A special issue of the Journal of Graph Theory was published in Frucht's honor in 1982,[2][10] and another special issue of the journal Scientia, Series A (the journal of the mathematics department of Federico Santa María Technical University) was published in honor of his 80th birthday in 1986.[2][11] </div>
How to suppress bullet points in HTML list
<ul> <li>(a) mines, quarries, and other works for the extraction of minerals from the earth;</li> <li>(b) industries in which articles are manufactured, altered, cleaned, repaired, ornamented, finished, adapted for sale, broken up or demolished, or in which materials are transformed; including shipbuilding and the generation, transformation and transmission of electricity or motive power of any kind;</li> <li>(c) construction, reconstruction, maintenance, repair, alteration, or demolition of any building, railway, tramway, harbour, dock, pier, canal, inland waterway, road, tunnel, bridge, viaduct, sewer, drain, well, telegraphic or telephonic installation, electrical undertaking, gas work, water work, or other work of construction, as well as the preparation for or laying the foundations of any such work or structure;</li> <li>(d) transport of passengers or goods by road, rail, or inland waterway, including the handling of goods at docks, quays, wharves or warehouses, but excluding transport by hand.</li> </ul> I have the above HTML. What CSS coding can I add above this HTML that will suppress the bullet points generated by the <li> tags?
Try following in your HTML, which will hide bullets of <li>:
<style>
ul {
list-style: none;
}
</style>
A Href on a new line
i have the following content <div class="venue-description"> <h4>Description</h4> Nandi Hills are currently undergoing a multi-crore development, including a one crore renovation of the Tipu Fort, via private-public partnership to transform the hills into a tourist hub. The Department of Horticulture is setting up a food court modeled after one in Singapore at a cost of nearly one crore at the hill station.Various varieties of vegetarian and continental food, beverages, bakery products, ice-creams and fresh fruit juices will be available. view more </div> I want to move the a tag to a new line. Using display: block will create a full width link which is bad for usability. i do not want to use a <br/> tag
DEMO
a::before {
content:'';
display:block;
}
Why dont you just put <br/> after <h4>Description</h4> Nandi Hills are currently undergoing a multi-crore development, including a one crore renovation of the Tipu Fort, via private-public partnership to transform the hills into a tourist hub. The Department of Horticulture is setting up a food court modeled after one in Singapore at a cost of nearly one crore at the hill station.Various varieties of vegetarian and continental food, beverages, bakery products, ice-creams and fresh fruit juices will be available.