Ripple Deep

Ripple Deep Retreats are held over one-day in a beautiful, serene garden venue right in the heart of East Fremantle. Our goal is to help nourish your body with yoga, and fresh juices and balance your mind and heart with breathing, deep relaxation practices, meditation and more! If you’re going through a tough time in life right now, or you just need some time to recharge and learn some life long skills, I definitely recommend you head along to a Ripple Retreat – it’s only one day but can affect a life time. Give the gift of relaxation, inner and wellness!

Enter the characters you see below Sorry, we just need to make sure you’re not a robot. Enter the characters you see below Sorry, we just need to make sure you’re not a robot. Would you hear my voice come through the music? Would you hold it near as it were your own? Let there be songs to fill the air. That was not made by the hands of men.

That path is for your steps alone. But if you fall you fall alone. If you should stand then who’s to guide you? If I knew the way I would take you home.

Thanks to Jim Burd, Sam D, Valentine, Reilly for correcting these lyrics. Grateful Dead lyrics are property and copyright of their owners. Ripple” lyrics provided for educational purposes and personal use only. Wave ripple or symmetric ripple, from Permian rocks in Nomgon, Mongolia.

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Note “decapatation” of ripple crests due to change in current. While wave-formed ripples are traditionally described as symmetrical, asymmetric wave ripples are common in shallow waters along sandy shores. They are produced by bottom oscillations generated by passing breaker waves, which have unequal intensity in opposite directions. Wave-formed ripples indicate an environment with weak currents where water motion is dominated by wave oscillations. Although symmetrical ripples are also called bi-directional ripples there is a difference between them. Bi-directional ripples are rarely symmetrical due to the difference in force of the two directions, where as the wave formed or oscillation ripples form from the circular water movement pattern of water molecules.

These ripples form parallel to the shore line. They usually display rounded troughs and rounded crests. Ripples are relatively small, elongated ridges that form on bed surfaces perpendicular to current flow. With continuous current flow in one direction, asymmetrical ripples form.

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Asymmetrical ripples contain a steeper slope downstream. With an alternation in current flow from one direction to the opposite symmetrical ripples form. Symmetrical ripples tend to have the same slope on both sides of the crest. Symmetrical ripples form as water molecules oscillate in small circles. A particle of water within a wave does not move with the wave but rather it moves in a small circle between the wave crest and wave trough. This movement of water molecules is the same for all water molecules effected by the wave. Wikimedia Commons has media related to Ripple marks.

The Changing Earth: Exploring Geology and Evolution, 2nd ed. 1997, Sea-floor geology of a part of Mamala Bay, Hawaii: Pacific Science, v. Chapter 7: A Surface Veneer: Sediments, Soils and Sedimentary Rocks. This article may require cleanup to meet Wikipedia’s quality standards. No cleanup reason has been specified. In physics and engineering, a ripple tank is a shallow glass tank of water used in schools and colleges to demonstrate the basic properties of waves.

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It is a specialized form of a wave tank. Ripples may be generated by a piece of wood that is suspended above the tank on elastic bands so that it is just touching the surface. Screwed to wood is a motor that has an off centre weight attached to the axle. As the axle rotates the motor wobbles, shaking the wood and generating ripples. A number of wave properties can be demonstrated with a ripple tank.

These include plane waves, reflection, refraction, interference and diffraction. When the rippler is attached with a point spherical ball and lowered so that it just touches the surface of the water, circular waves will be produced. When the rippler is lowered so that it just touches the surface of the water, plane waves will be produced. By placing a metal bar in the tank and tapping the wooden bar a pulse of three of four ripples can be sent towards the metal bar. The ripples reflect from the bar. If the bar is placed at an angle to the wavefront the reflected waves can be seen to obey the law of reflection. The angle of incidence and angle of reflection will be the same.

If a concave parabolic obstacle is used, a plane wave pulse will converge on a point after reflection. This point is the focal point of the mirror. Circular waves can be produced by dropping a single drop of water into the ripple tank. If this is done at the focal point of the “mirror” plane waves will be reflected back.

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If a sheet of glass is placed in the tank, the depth of water in the tank will be shallower over the glass than elsewhere. The speed of a wave in water depends on the depth, so the ripples slow down as they pass over the glass. This causes the wavelength to decrease. If the junction between the deep and shallow water is at an angle to the wavefront, the waves will refract. In practice, showing refraction with a ripple tank is quite tricky to do.

The sheet of glass needs to be quite thick, with the water over it as shallow as possible. This maximizes the depth difference and so causes a greater velocity difference and therefore greater angle. If the water is too shallow, viscous drag effects cause the ripples to disappear very quickly. The glass should have smooth edges to minimise reflections at the edge.

Ripple Deep

If a small obstacle is placed in the path of the ripples, and a slow frequency is used, there is no shadow area as the ripples refract around it, as shown below on the left. A faster frequency may result in a shadow, as shown below on the right. If a large obstacle is placed in the tank, a shadow area will probably be observed. If an obstacle with a small gap is placed in the tank the ripples emerge in an almost semicircular pattern. If the gap is large however, the diffraction is much more limited.

Small, in this context, means that the size of the obstacle is comparable to the wavelength of the ripples. A phenomenon identical to the x-ray diffraction of x-rays from an atomic crystal lattice can also be seen, thus demonstrating the principles of crystallography. Interference can be produced by the use of two dippers that are attached to the main ripple bar. In the diagrams below on the left the light areas represent crests of waves, the black areas represent troughs. Notice the grey areas: they are areas of destructive interference where the waves from the two sources cancel one another out. To the right is a photograph of two-point interference generated in a circular ripple tank. Visit Campbell River Tourism’s profile on Pinterest.

Ripple Deep

The History of Campbell River The Tides of Time Long before European explorers entered the waters surrounding Campbell River, the First Nations people lived here in harmony with nature, and the cycles of the salmon. K’u ta’la-which had spiritual significance and was honoured through art and ceremony. It’s suggested that European explorers arrived in this region as early as the late 1500s, when Sir Francis Drake over-wintered just south of where Campbell River is today. Two centuries later, in 1778, Captain James Cook came ashore at Friendly Cove in Nootka Sound. In 1792, Captain George Vancouver landed on Quadra Island. He also named many local landmarks, including Discovery Passage, which you see today from Campbell River’s waterfront. Permanent settlement in Campbell River and the Discovery Islands occurred during the 1880s, changing the way salmon was harvested.

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The area first received international sport fishing acclaim in 1896, when Sir Richard Musgrave detailed his accounts in the British magazine, The Field. You can still become a member. The mighty Tyees are the stuff of which legends-and great fish stories-are made. The region also developed forestry, mining, and other enterprises, including a whaling station on Cortes Island and a fish cannery on Quadra Island. In 1952, Elk Falls pulp and paper mill opened on a point of land jutting into Discovery Passage.

This state-of-the-art facility is now Campbell River’s largest employer, and during the summer, mill tours are available. As commercial activity grew, so did concern for conservation, and in 1911, Strathcona Provincial Park was created to protect the surrounding natural heritage. In the relatively short time since permanent settlers arrived here, Campbell River has changed dramatically, and it’s now home to over 31,000 residents. But below the high water mark, the cycles of the salmon continue as they have for thousands of years. Campbell River celebrates and perpetuates this heritage with successful salmon stream enhancement projects, numerous ecological and recreational greenways, a meandering oceanside walkway, museums and cultural programs, and more. Explore Campbell River’s past through the writings and heritage home of Roderick Haig-Brown, renowned twentieth century sport fisher and nature conservationist. Haig-Brown was also an acclaimed outdoors writer.

During his lifetime, he published numerous articles and over twenty-five books, some of which are still in print-others, as you might imagine, are treasured collector’s items. Haig-Brown’s deep respect for nature, waterways, fish, and in particular, salmon, lives on today not only through his writings, but also through his conservation efforts. Over the years, Haig-Brown and his wife Ann worked to preserve several of British Columbia’s natural legacies. Today, you can visit the Haig-Brown family home in Campbell River. Since 1990, the house, gardens and orchard have been an official British Columbia Heritage Site. Tour Haig-Brown’s inspiring library, the riverside grounds, and the adjacent Haig-Brown Kingfisher Creek salmon enhancement project.

Plan to linger awhile-it’s also a charming bed and breakfast. The Tyee Club Re-live Campbell River’s legendary sport fishing days by joining the famed Tyee Club. Strict rules stipulate that, among other things, you fish from a rowboat in Discovery Passage’s Tyee Pool with a hand-operated reel and no more than twenty-pound test line. Today, this venerable institution also participates in salmon enhancement and waterway restoration projects. For more information, telephone the Tyee Club at 250-287-2724.

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Book your Tyee Rowing Guide to experience this traditional style of salmon fishing first hand. In Campbell River, the Salmon Capital of the World, Painter’s Lodge is a sportfishing icon. It opened in the 1920s with a few rustic cabins operated by Ned and June Painter on Campbell River Spit. Ned Painter was also associated with the famous Tyee Club and built wooden rowboats that he rented and sold to anglers. In 1938, the Painters moved their operation to the oceanfront where the resort now stands. June Painter worked steadfastly to ensure its success, and after ten years in their new location, the family sold the lodge.

Tragically, in 1985 fire destroyed the historic lodge and its irreplaceable memorabilia. Before long though, Painter’s Lodge was rebuilt. Over the years, Painter’s-as it’s fondly called-has hosted Hollywood celebrities like John Wayne, Bing Crosby and Bob Hope and many others aspiring to join the legendary Tyee Club. This renowned resort continues to welcome guests to the community. Ripple Rock – The Devil Beneath the Sea Until 1958, the Devil Beneath the Sea lurked just north of Campbell River. It wasn’t actually a sea monster, it was treacherous Ripple Rock, which lay concealed in seething tidal currents at the mouth of Seymour Narrows.

It was a navigational hazard, and over a hundred ships and just as many souls met their fate on its unforgiving shoulders. Over the years, there were several unsuccessful attempts to remove Ripple Rock. By the mid-1950s, however, engineers had devised an elaborate plan that involved sinking a shaft through nearby Maud Island, tunneling horizontally under Ripple Rock, then up into its twin peaks. Working non-stop, it took miners twenty-eight months to drill the tunnels and install explosives.

In 1958, the day of the big blast arrived. It was the largest man-made, non-nuclear explosion in history, a record that stands to this day. As dust and debris fell back to earth, the Devil Beneath the Sea disappeared forever into the murky depths. There’s a viewpoint on Highway 19 just north of Campbell River, and a trail near the site of Ripple Rock. Vancouver Island, BC has been voted North America’s Best Island, a Reader’s Choice Award, by Conde Nast Traveler Magazine readers for 9 consecutive years. Ch 3, make 13 DC in loop, join.

DC in base of starting Ch 3, Ch 2, join. Round 3: Sl St in first V-stitch space, chain 3, DC-Ch2-2DC in same space. Rounds 7-16: Repeat round 6 ten more times. Ch 3, 9 DC in loop, join. Round 2: Ch 3, DC in same st. DC in next st, 2DC in next st.