Current Time On The Rock
Saturday, January 31, 2009
"Lookin"
"Put-In, Quidi Vidi Newfoundland"
"Gut Return"
"Outside The Gut, Of Quidi Vidi"
Quidi Vidi Ice"
"Good Mooring"
Friday, January 30, 2009
"Black Water"
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I am moved by the colors of water I believe. Perhaps it is because they represent or reflect, to some extent, what is going on in the environment around you at the time. When we add the color to the concept of wave we can even get another mood alteration or emotional switch.Water is water, it is still wet no matter the color, it will still freeze given the right temperature and depending on salinity. How does frozen water affect your mood? I enjoy all the colors of water I paddle in and I allow them to affect my mood and sometimes look forward to their colors and their ways because it is after all the medium for kayak travel and as much as we are enticed by the colors of our boats and our gear so too can we be moved by our travelling medium.
Saturday, January 24, 2009
"Sea Ice Data.....Around Newfoundland"
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More to ice than meets the eye may be an understatement. As I was reading up on sea ice I discovered new terminology and the "Egg Code" which is used to describe ice concentration, the stage of ice and the size of ice floes using coded numbers. At first I found it a bit difficult but wih some practise I was able to gain a very, very basic understanding of the concept. I found it an extremely interesting exercise none-the-less.
Sea-ice types New: A general term for recently formed ice which includes frazil ice, grease ice, slush and shuga. These types of ice are composed of ice crystals which are only weakly frozen together (if at all) and have a definite form only while they are afloat.
Grey: Young ice 10-15 cm thick. Less elastic than nilas and breaks on swell. Usually rafts under pressure.
Grey-white: Young ice 15-30 cm thick. Under pressure it is more likely to ridge than to raft.
Thin first-year: First-year ice of not more than one winter's growth, 30-70 cm thick.
Medium first-year: First-year, ice 70-120 cm thick.
Thick first-year: First-year ice over 120 cm thick.
Old ice: Sea ice which has survived at least one summer's melt. Topographic features generally are smoother than first-year ice. May be subdivided into second-year ice and multi-year ice.
Second-year ice: Old ice which has survived only one summer's melt.
Multi-year ice: Old ice which has survived at least two summer's melt.
Lake-ice types
New: Recently formed ice less than 5 cm thick.
Thin: Ice of varying colours, 5-15 cm thick.
Medium: A further development of floes or fast ice, 15-30 cm thick.
Thick: Ice 30-70 cm thick.
Very Thick: Floes or fast ice developed to more than 70 cm thickness.
Arrangement of the ice
Ice drift: Caused by the combined action of the wind and water current's drag on the ice. Expressed in units of kilometres per day (km/d). Terms used are descriptive: slow or light, moderate, rapid, and variable.
Ice growth: Caused by the freezing of water by cold air, and its rate will depend on the air temperature, wind conditions, and water salinity. Terms used are descriptive: little or no ice growth, slow or light, moderate, and rapid.
Ice melt: Caused by the melting of ice by warm water or warm air. Terms used are descriptive: slow or light, moderate, and rapid.
Ice pressure: Caused by compaction of ice floes under the influence of wind or water currents, forming ice deformation of several forms (fractures, hummocks, ridges, rafting). Terms used are descriptive: light, moderate, strong.
Ice concentrations
The ratio expressed in tenths describing the amount of the water surface covered by ice as a fraction of the whole area.
Ice free: No ice present. If ice of any kind is present, this term shall not be used.
Open water: A large area of freely navigable water in which ice is present in concentrations less than 1/10. No ice of land origin is present.
Drift ice/Pack ice: Term used in a wide sense to include any area of ice, other than fast ice, no matter what form it takes, or how it is disposed. When concentrations are high, i.e., 7/10 or more, drift ice may be replaced by the term pack ice.
Very open drift: Ice in which the concentration is 1/10 to 3/10 and water dominates over ice.
Open drift: Floating ice in which the concentration is 4/10 to 6/10, with many leads and polynyas. Floes generally not in contact with one another.
Close pack: Floating ice in which the concentration is 7/10 to 8/10, composed of floes mostly in contact with one another.
Very close pack: Floating ice in which the concentration is 9/10 to less than 10/10.
Compact ice: Floating ice in which the concentration is 10/10 and no water is visible.
Consolidated ice: Floating ice in which the concentration is 10/10 and the floes are frozen together.
Ice distribution
The following terms are used in ice messages and forecasts to describe the distribution of ice in a given area.
Ice cake: Any relatively flat piece of ice less than 20 m across.
Ice Openings: Includes all forms of fractures and cracks.
Crack: Any fracture of fast ice, consolidated ice, or a single floe which may have been followed by separation ranging from a few centimetres to 1 m.
Strips: Long narrow area of drift ice, about 1 km or less in width, usually composed of small fragments detached from the main mass of ice, which run together under the influence of wind, swell or current.
Ice edge: The demarcation at any given time between the open water and sea, lake or river ice whether fast or drifting. May be termed compacted or diffuse.
Iceberg concentrations and limits
Isolated: No more than one iceberg per degree of latitude and longitude.
Scattered: Two to four icebergs per degree of latitude and longitude.
Many: Five to ten icebergs per degree of latitude and longitude.
Numerous: More than 10 icebergs per degree of latitude and longitude.
Limit of all known icebergs: The limit at any given time between iceberg infested waters (with or without sea ice) and ice-free waters.
Wednesday, January 21, 2009
"Kayaking Dreamin'"
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Saturday, January 17, 2009
"Girls To The Park..."
Thursday, January 15, 2009
"Obstacles??????"
Some obstacles are big, really big they are hard to move or even avoid. So what do we do? What do you do when you face an obstacle? Do we think it through? Do we have time to think it through? Could we have minimized, prevented? When we kayak there are many obstacles. I am sure even that everyone would most likely deal with the same ones differently. Take for instance outfitting your kayak so that it is snug yet comfortable enough for you to roll. I garauntee everyone would have a spin on how it should be done, but the end result should be the same .......to roll efficiently or in some cases just to roll, which is fine. What is the obstacle? The inabiltiy to outfit the cockpit porperly, inadequate learning, or maybe learning it wrong and it doesn't really matter because they are all obstacles to rolling.
I am under the impression that to be a decent paddler you have to over come so many obstacles and many created by our own course of actions or mind set perhaps. What if you were faced with the same obstacle everyday or on every paddle or on every adventure (maybe a mental obstacle)...what would you do? I would adapt. Like in this picture.....obviously I am not going through the rock......I will go around it. I will adapt my forwward progress. Should we train ourselves to adapt to obstacles or to avoid them? Or is it that black and white?
Tuesday, January 13, 2009
Sunday, January 11, 2009
"Holyrood, Newfoundland"
In 1969 the Town of Holyrood incorporated.
It was a nice place to paddle today in calm waters and a low wind. The water was 1 degree celsius and the air was about zero. A great paddle with my friend Tony on a Sunday morning. As David Francey says in one of his songs, "Way off in the distance there rang a bell and it rang for the Saints and the Sinners as well..."
"Frozen Steer head?"
"The Very Rare.....The Ivory Gull"
"Into The Icey Jaws"
"Milions and Millions and Millions...."
"Chapel Cove"
"Show Me The Way"
Saturday, January 10, 2009
"Petty Harbour, Newfoundland"
Petty Harbour also has some claim to fame in the film industry. Such movies as; "Hatching, Matching and Dispatching", "Orca", "A Whale Of A Tale", "Rare Birds", "John and THe Mrs", and parts of "The Terry Fox Story" have all had some involvement in this small friendly place you can access on the way to the Cape Spear Lighthouse, the most Eastern location in North America.
Alan Doyle of "Great Big Sea" a successful band from Newfoundland is from the Town of Petty Harbour.
It is hard not to be charmed by the community and even easier to enjoy a decent paddle just inside and outside the protecting walls of her harbour.
Friday, January 09, 2009
"Paddlin' Buds"
Thursday, January 08, 2009
"Bay Bulls, Newfoundland"
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Warfare History:
In a 150 year span from about 1650 until 1800, Bay Bulls was the site of numerous conflicts between various European nations. In 1655, the tiny community was raided by Dutch sailors under Admiral De Ruyter and while the town was looted and pillaged, it was rebuilt almost immediately. In the 100 years between 1696 and 1796 Bay Bulls was attacked at least five times by the French military via land and sea. These attacks were often in conjunction with attacks on St. John's in part of the French effort in the early eighteenth century to drive the English out of Newfoundland.
Two of the more memorable battles took place in 1696 when Monbeton de St. Ovide de Brouillan, the governor of Placentia (another Newfoundland community), attacked Bay Bulls from the sea and in 1697 when Pierre Le Moyne d'lberville marched overland. In the first skirmish a British frigate, The HMS Sapphire, was scuttled in order to prevent the ship from falling into enemy hands. The Sapphire is now depicted in the official town logo and can still be seen in the harbour During periods of low tide. The site was declared Newfoundland and Labrador's first underwater marine historic site in 1975.
In 1705 an expedition of 90 Frenchmen and 100 Indians on its way from Placentia to attack St. John's, captured Bay Bulls. Once again the town was put to the torch before the French left. Two years later Bay Bulls was again captured by the French and this time there was no resistance from the settlers. The attack of 1707 was the last enemy evasion until June 24, 1762 when the French lead by Admiral De Terne, landed seven hundred men who occupied Bay Bulls and marched to St. John's. The French later left rather than fight the British forces sent against them, and Bay Bulls was rebuilt once again.
On September 29, 1796 Bay Bulls suffered its last invasion when an Admiral Richery attempted to storm St. John's but finding it well defended, attacked and burned Bay Bulls instead and took prisoners. He was eventually driven out as well and the community quickly recovered.
Reprinted from Bay Bulls website.
Wednesday, January 07, 2009
"Sweet Product"
Tuesday, January 06, 2009
"To Top It Off..."
Sunday, January 04, 2009
"Newfoundland and Labrador"
I saw this on the way up Signal Hill today. Fresh Snow and Sunshine made these black statues of a Labrador Retriever and Newfoundland dog contrast nicely. Would have been a good few hours of sunshine for the water but I just got off work and decided on fastfood and dining at the top of Signal Hill for the view. There were low lying clouds raining off in St. John's Bay with the sun pouring down everywhere else. Also looked like huge swell out there. A beautiful day on the Island.
"Gull Respite"
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