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>
<div class="clear"></div>
<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>
<div class="clear"></div>
<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>
<div class="clear"></div>
<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>
<div class="clear"></div>
<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>
<div class="clear"></div>
<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.
I'm creating a website in WordPress, it's going well, but whenever I try to add pictures to the page of the site, the text won't wrap around them. The pages are supposed to be created when you're inside of your WP account, so there is minimal coding involved, and each page has it's own coding and formatting as far as html is concerned. I would be willing to change the CSS to fix this problem, but I wouldn't know where to start. Here is the code for the About Us page:
Cougar Electric Car Company is made up of students at
Kennedy High School in Cedar Rapids, Iowa. Students work in teams to design and construct safe, energy-efficient electric one-person vehicles that they showcase during a series of rallies across the
Midwest. This is hands-on education. Team members apply what they’ve learned in math science, and or vocational education – and more.
<img style="float: right;" src="http://leifsegen.com/sandbox/livia_t/electric-car/wordpress/wp-content/uploads/2016/02/IMG_5139-300x225.jpg" alt="IMG_5139" width="300" height="225" />
<h6>The program is designed to challenge students to:</h6>
<ul>
<li>Apply classroom lessons to build a one-person light electric vehicle</li>
<li>Design and engineer the vehicle to roll safely and efficiently</li>
<li>Use problem-solving skills</li>
<li>Promote efforts in the community to gain support</li>
<li>Compete against other schools to see whose vehicle performs best</li>
<li>Document the design/build/compete process</li>
</ul>
<h6><strong>Since 1997</strong></h6>
The program was launched by two students and Kennedy teacher Barry Wilson in 1997. Since then, the program has impacted hundreds of students and sparked interest in manufacturing, engineering, automotive, alternative energy, and many more career paths.
Here is the link to my About Us page.
From your linked page, it looks like your img tag is within a distinct paragraph tag underneath another paragraph tag. Since paragraph tags are block elements, they stack instead of allowing inline flow.
to resolve this, you want to go to the edit post/page area, and place the media at the start of the paragraph you want wrapping around it (or, however many lines down you want to start the wrapping). Click the image, then select the box that looks like a box w lines wrapping around it. See my screenshot for an example
You can accomplish the same thing in text mode instead of visual editor mode by placing the image tag within the same paragraph tag that the paragraph is in, then giving it a float:right / left property
Move the image inside the <ul> that will solve your issue. Already tested and its working
<ul>
<li style="list-style: none;"><img style="float: right;" src="http://leifsegen.com/sandbox/livia_t/electric-car/wordpress/wp-content/uploads/2016/02/IMG_5139-300x225.jpg" alt="IMG_5139" width="300" height="225"></li><li>Apply classroom lessons to build a one-person light electric vehicle</li>
<li>Design and engineer the vehicle to roll safely and efficiently</li>
<li>Use problem-solving skills</li>
<li>Promote efforts in the community to gain support</li>
<li>Compete against other schools to see whose vehicle performs best</li>
<li>Document the design/build/compete process</li>
</ul>
<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>
I've got a HTML document within an iframe that people will be printing off, I've coded it to look good when it prints. There's a footer and a header, the header changes for each page and each page is within it's own div tag. I want people to be able to hit the print button for the document and the pages each print on their own page without getting cut off and making sure the footer stays at the bottom of each page. Is there a way to do this? I'd love some help with this as it's driving me crazy! It looks like crap when like a page is too short so the next page will print on the same page and then get cut off halfway through.
This is where I have it set up..
http://morecleanenergy.com/graphics/testproposal/index.html
Here is one of the pages..
<div style="size:210mm 297mm;">
<table width="100%" border="0" cellpadding="0" cellspacing="0" class="Proposalheader">
<tr>
<td align="left" width="169"><img src="faq.png" height="57px"></td>
<td width="732"></td>
</tr></table>
<div class="pageBody">
<span class="generalText"><p><strong>Who is Clean Energy Collective?</strong></p>
<p>Clean Energy Collective (CEC) is a Colorado-based company that develops, operates and maintains community-owned solar arrays, also referred to as solar gardens or community solar farms. CEC's innovative model makes local renew- able energy easy, accessible and a financially smart decision for electricity consumers in the United States.</p>
<p><strong>What is CEC Community Solar?</strong></p>
<p>Clean Energy Collective community solar enables you to own solar panels in a centralized, community-based array. As your panels produce clean electricity, you receive credits directly on your monthly electric bills for the power produced. By owning a solar power system in a community array, you can reduce or eliminate your electric bills, protect against rising prices, and experience monthly savings in place of a monthly expense.</p>
<p><strong>What happens to the electricity produced by the panels?</strong></p>
<p>The clean solar power is automatically delivered to the Xcel Energy's grid, increasing the utility's incorporation of renewable energy and decreasing its reliance on fossil fuels. The power is not delivered directly to your meter and no equipment is required to be installed on your property.</p>
<p><strong>Do I need to own a home or building to participate?</strong></p>
<p>No. If you have an electric bill, you can receive credits for the power produced by solar panels in a CEC communi- ty-owned solar array.</p>
<p><strong>How can I monitor my panels' performance?</strong></p>
<p>As a CEC customer, you can log on to your My Own Clean Energy account via the CEC website and smartphone app. There you can see your system's information, review your customer documents, and access real-time information about your portion of the array's production, bill credits, and positive environmental impact.</p>
<p><strong>What happens if I move?</strong></p>
<p>If you move within your county, simply have your panels' bill credits applied to your new location's meter and account with the utility. If you leave the county or the Xcel Energy territory, you may sell the panels to another Xcel Energy customer in your county or give a tax-deductible gift of clean energy by donating the system to a charity in your county.</p>
<p><strong>How much solar can I buy?</strong></p>
<p>Systems are available from a minimum of 1 kilowatt (kW) up to 120% of your average annual usage.</p>
<p><strong>How are my monthly electric bill credits calculated?</strong></p>
<p>Each month, your Xcel Energy electric bill will be credited for your panels' production. The power produced is credited at the specific rate for your customer class as determined under Xcel Energy's Solar*Rewards Community Program. These initial credit rates will increase as Xcel Energy's electricity rates increase, protecting you against the national trend of rising electricity costs.</p>
<p><strong>How are my monthly electric bill credits calculated?</strong></p>
<p>As Xcel Energy's electricity prices rise, the bill credit rate you receive for the panels' output will increase as well. As your monthly bill credits increase, your system's savings increase.</p></span>
</div>
<div><img src="footer.png" style="width:100%;"></div>
</div>
Try applying the page-break-after css property to your footer. http://www.w3schools.com/cssref/pr_print_pageba.asp
This question already has an answer here:
CSS Show Hide Only
(1 answer)
Closed 8 years ago.
The design of my website is integrated within their company. Basically they are rebranding their website with my information and logo. They want extra money to change any HTML files. I only have access to the stylesheets .css files and images. I have tried the hover in css but I would like it to remain open if clicked on. OR hover and delayed before closing
Can I make a css show/hide with the h3 listed in the sample below: I would like to hide the content under each h3 until the user clicks on it. I have shortened the HTMl I pulled from the product page for sample purposes.
<div id="product_text_content">
<p>Digital Brochures come in full color on 1 or 2 sides. Available options: 8 paper stocks, 5 sizes, and 3 coatings.</p>
<h3 class="gray">SIZE:</h3>
<ol>
<li>8.5" x 11"</li>
<li>8.5" x 14"</li>
<li>11" x 17"</li>
<li>11.5" x 17.5"</li>
<li>5.5" x 8.5"</li>
</ol>
<h3 class="gray">PAPER OPTIONS:</h3>
<ol>
<li>100# Gloss Text available</li>
<li>95# Gloss Cover available</li>
<li>80# Uncoated Offset Smooth Text</li>
<li>100# Uncoated Cover available</li>
<li>70# White Linen Text</li>
<li>100# White Linen Cover</li>
</ol>
<h3 class="gray">COATING OPTIONS:</h3>
<ol>
<li>No Coating available on all stocks.</li>
</ol>
<h3 class="gray">FOLDING OPTIONS:</h3>
<ol>
<li>Tri-Fold</li>
<li>Z-Fold</li>
<li>... and more</li>
</ol>
<h3>Custom Estimate:</h3>
<p>For custom orders or quantities not listed for your desired product, please click here for a custom estimate.</p>
<h3>Explanation of Turnaround Time</h3>
<p>Here's a quick chart to explain turnaround times:</p>
<img src="/img/products/turnaround.png" height="375" width="380">
<p>Please note that turnaround time does not include shipping or mailing time. You may select from available production turnaround times and your preferred shipping time as you place your order.</p>
<p>Turnaround times begin when the proof is approved. All times are based on standard business days Monday through Friday excluding federal holidays. For orders shipping to the <font color="blue">blue zone</font>, please use the Eastern time zone (New York). For orders shipping to the <font color="red">red zone</font>, please use the Pacific time zone (California). Please see the below map:</p>
<img src="/img/products/map.jpg" height="155" width="300">
<p>Our products are the same great quality for every turnaround time we offer.</p>
To toggle data on and off (show and hide in this case), you will need to use js/jquery. This can only be called through HTML, so I'm afraid you might have to bite the bullet and pay for HTML access.