You will also reflect on your previous work experience and potential career in Land Business. Please note: You are required to attend 1 lecture class, noted below.

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The rest of this course is self-directed study. Course materials: available at the Campus Store. Workplace Presentation Skills For most people, delivering a presentation is nerve-racking.

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  • Acquire tools and techniques to increase your comfort and effectiveness in giving presentations. Please note: This course is mandatory for program completion as of Winter Students who started the PLB program prior to Winter are not required to complete this course. Mineral Rights and Regulations Overview Explore the principle features, standard clauses, formalities of completion and execution, and termination of freehold and crown mineral leases while examining common regulatory and legal issues.

    Surface Rights and Regulations Overview Examine how the surface land department works, the ins-and-outs of regulatory bodies, and the land process from exploration to site abandonment. Learn techniques for formulating strategies and applying them to business situations. Prerequisite: Mineral Rights and Regulations Overview. Economics and Petroleum Asset Evaluation Apply economic principles and risk analysis to structure and evaluate land deals while exploring alternative value measurement methods. Land Agreements Examine the structures and contractual obligations of common exploration agreements, joint operating agreements and unit agreements.

    Land Negotiations Review explorations, land and joint agreements, identify problems in contracts, justify interests and draft special clauses. Learn about farm-in, farm-out, pooling and disposition negotiations. Prerequisite: Land Agreements. Prerequisite: Previous 12 Petroleum Land Business courses Course materials : Distributed in class throughout this course.

    Real Estate Address Change on Land Title In Calgary, Alberta

    Jim spent five years on the Board of the Canadian Association of Petroleum Landmen where he was President in Jim has a strong knowledge base in Land organization, management and related functions with particular expertise in Subsurface Mineral Land Negotiations. Jim is a native of Calgary, Canada. He has a penchant for volunteering and has been involved in several organizations in many capacities including on various boards and as a coach for sports and organizations such as hockey and football, the YMCA and more.

    Jim is married to Pat with three maturing young adults as family. Curt Hamrell Curt has been working in the oil and gas industry since Curt is a firm believer in education and enjoys teaching at a place where he formerly was a student. Curt has been a teacher in Land courses for the past plus years. He has also taught at Olds College and taught in-house Land seminars at various oil and gas companies.

    Curt has been married for plus years with two teenaged daughters. Gary Lepine Dr. Gary Lepine has been providing ethics seminars and professional development for a variety of associations and companies for the past 12 years. Gary is also co-founder of Finishing Well, an organization that offers public education on advance care planning and living with a terminal or critical illness. Nikki Sitch Ms.

    She is a Petroleum Landman with over 17 years of experience in all facets of Land management in the Canadian western sedimentary basin. She has gained knowledge and experience in exploration, development, as well as acquisitions and divestitures, in both Surface and Mineral Land, in the producing regions of Western Canada.

    For the past five years Ms. Sitch has a passion for learning and education. She enjoys giving back to the Land community through teaching and mentoring. Her career has spanned across all facets of land management, deal negotiation, contract drafting, mineral and surface analysis, administration, and acquisitions and divestitures.

    Her geographic experience in agreement writing and negotiation ranges from the Western Canadian Sedimentary Basin to the offshore and frontier regions of Canada, the United States and internationally. Lenni currently holds the position of Land Manager at a junior oil and gas company.

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    She has held key positions with major, intermediate and junior energy companies. Lenni has developed and presented in-house Land Contracts seminars for her oil and gas clients and employers.

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    She has enjoyed roles in teaching, mentoring and curriculum advisory at the Southern Alberta Institute of Technology and Mount Royal University. Lenni is passionate about facilitating quality adult education at Mount Royal University. The northern and western parts of the province experience higher rainfall and lower evaporation rates caused by cooler summer temperatures.

    The south and east-central portions are prone to drought-like conditions sometimes persisting for several years, although even these areas can receive heavy precipitation, sometimes resulting in flooding. In southwestern Alberta, the cold winters are frequently interrupted by warm, dry chinook winds blowing from the mountains, which can propel temperatures upward from frigid conditions to well above the freezing point in a very short period.

    Northern Alberta is mostly covered by boreal forest and has a subarctic climate. The agricultural area of southern Alberta has a semi-arid steppe climate because the annual precipitation is less than the water that evaporates or is used by plants. The southeastern corner of Alberta, part of the Palliser Triangle , experiences greater summer heat and lower rainfall than the rest of the province, and as a result suffers frequent crop yield problems and occasional severe droughts.

    Western Alberta is protected by the mountains and enjoys the mild temperatures brought by winter chinook winds.

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    Central and parts of northwestern Alberta in the Peace River region are largely aspen parkland, a biome transitional between prairie to the south and boreal forest to the north. After Saskatchewan, Alberta experiences the most tornadoes in Canada with an average of 15 verified per year.

    In central and northern Alberta the arrival of spring is marked by the early flowering of the prairie crocus anemone ; this member of the buttercup family has been recorded flowering as early as March, though April is the usual month for the general population. Both yellow and white sweet clover can be found throughout the southern and central areas of the province. The trees in the parkland region of the province grow in clumps and belts on the hillsides. These are largely deciduous , typically aspen , poplar , and willow.

    Many species of willow and other shrubs grow in virtually any terrain. On the north side of the North Saskatchewan River evergreen forests prevail for thousands of square kilometres. Aspen poplar , balsam poplar or in some parts cottonwood , and paper birch are the primary large deciduous species. Conifers include jack pine , Rocky Mountain pine, lodgepole pine , both white and black spruce , and the deciduous conifer tamarack.

    The four climatic regions alpine , boreal forest , parkland , and prairie of Alberta are home to many different species of animals. The south and central prairie was the land of the bison , commonly known as buffalo, its grasses providing pasture and breeding ground for millions of buffalo. The buffalo population was decimated during early settlement, but since then buffalo have made a comeback, living on farms and in parks all over Alberta. Herbivorous animals are found throughout the province. Moose , mule deer , elk , and white-tailed deer are found in the wooded regions, and pronghorn can be found in the prairies of southern Alberta.

    Bighorn sheep and mountain goats live in the Rocky Mountains. Rabbits, porcupines , skunks , squirrels and many species of rodents and reptiles live in every corner of the province. Alberta is home to only one variety of venomous snake, the prairie rattlesnake. Alberta is home to many large carnivores. Among them are the grizzly bears and black bears , which are found in the mountains and wooded regions. Smaller carnivores of the canine and feline families include coyotes , wolves , fox, lynx , bobcat and mountain lion cougar. Central and northern Alberta and the region farther north is the nesting ground of many migratory birds.

    Vast numbers of ducks , geese , swans and pelicans arrive in Alberta every spring and nest on or near one of the hundreds of small lakes that dot northern Alberta. Eagles , hawks , owls and crows are plentiful, and a huge variety of smaller seed and insect-eating birds can be found.

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    Alberta, like other temperate regions, is home to mosquitoes , flies , wasps , and bees. Rivers and lakes are populated with pike , walleye , whitefish , rainbow , speckled , brown trout , and sturgeon. Bull trout , native to the province, is Alberta's provincial fish. Turtles are found in some water bodies in the southern part of the province. Frogs and salamanders are a few of the amphibians that make their homes in Alberta. Alberta is the only province in Canada—as well as one of the few places in the world—that is free of Norwegian rats. In , Alberta Agriculture reported zero findings of wild rats; the only rat interceptions have been domesticated rats that have been seized from their owners.

    It is illegal for individual Albertans to own or keep Norwegian rats of any description; the animals can only be kept in the province by zoos, universities and colleges, and recognized research institutions.


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    In , several rats were found and captured, in small pockets in southern Alberta, [33] putting Alberta's rat-free status in jeopardy. A colony of rats were subsequently found in a landfill near Medicine Hat in , and again in Alberta has one of the greatest diversities and abundances of Late Cretaceous dinosaur fossils in the world. At least 38 dinosaur type specimens were collected in the province. Dinosaur-bearing strata are distributed widely throughout Alberta.

    In the central and southern regions of Alberta are intermittent Scollard Formation outcrops. Other formations have been recorded as well, like the Milk River and Foremost Formations. However, these latter two have a lower diversity of documented dinosaurs, primarily due to their lower total fossil quantity and neglect from collectors who are hindered by the isolation and scarcity of exposed outcrops. Their dinosaur fossils are primarily teeth recovered from microvertebrate fossil sites. Additional geologic formations that have produced only few fossils are the Belly River Group and St.

    Mary River Formations of the southwest and the northwestern Wapiti Formation. The Wapiti Formation contains two Pachyrhinosaurus bone beds that break its general trend of low productivity, however. The Bearpaw Formation represents strata deposited during a marine transgression. Dinosaurs are known from this formation, but represent specimens washed out to sea or reworked from older sediments.