Pronunciation problems I have encountered as an English teacher and introduces some innovative, yet simple, practice techniques. The main goal of Pronunciation Keys is to help you develop more natural-sounding speech so that you will be able to understand more of what you hear. This system is based on two fundamental beliefs: 1. Top Notch Third Edition Classroom Audio Program Here are the audio resources to accompany the Student's Book. If you have any problems playing or downloading these files, please contact us online.

• Natural English Moving 1 Pdf Word
• Natural English Moving 1 Pdf Free
• Natural English Moving 1 Pdf Converter

Hydrology (from Greek: ὕδωρ, 'hýdōr' meaning 'water'; and λόγος, 'lógos' meaning 'study') is the scientific study of the movement, distribution, and quality of water on Earth and other planets, including the water cycle, water resources and environmental watershed sustainability. A practitioner of hydrology is a hydrologist, working within the fields of earth or environmental science, physical geography, geology or civil and environmental engineering.^[1] Using various analytical methods and scientific techniques, they collect and analyze data to help solve water related problems such as environmental preservation, natural disasters, and water management.^[1]

Hydrology subdivides into surface water hydrology, groundwater hydrology (hydrogeology), and marine hydrology. Domains of hydrology include hydrometeorology, surface hydrology, hydrogeology, drainage-basin management and water quality, where water plays the central role.

Oceanography and meteorology are not included because water is only one of many important aspects within those fields.

AP® English Literature and Composition Teacher's Guide Ellen Greenblatt The Bay School San Francisco, California connect to college success™ www.collegeboard.com.

Hydrological research can inform environmental engineering, policy and planning.

• 4Themes
• 5Organizations

Branches[edit]

• Chemical hydrology is the study of the chemical characteristics of water.
• Ecohydrology is the study of interactions between organisms and the hydrologic cycle.
• Hydrogeology is the study of the presence and movement of groundwater.
• Hydroinformatics is the adaptation of information technology to hydrology and water resources applications.
• Hydrometeorology is the study of the transfer of water and energy between land and water body surfaces and the lower atmosphere.
• Isotope hydrology is the study of the isotopic signatures of water.
• Surface hydrology is the study of hydrologic processes that operate at or near Earth's surface.
• Drainage basin management covers water storage, in the form of reservoirs, and floods protection.
• Water quality includes the chemistry of water in rivers and lakes, both of pollutants and natural solutes.

Applications[edit]

Natural English Moving 1 Pdf Word

• Calculation of rainfall.
• Calculating surface runoff and precipitation.
• Determining the water balance of a region.
• Determining the agricultural water balance.
• Designing riparian restoration projects.
• Mitigating and predicting flood, landslide and drought risk.
• Real-time flood forecasting and flood warning.
• Designing irrigation schemes and managing agricultural productivity.
• Part of the hazard module in catastrophe modeling.
• Providing drinking water.
• Designing dams for water supply or hydroelectric power generation.
• Designing bridges.
• Designing sewers and urban drainage system.
• Analyzing the impacts of antecedent moisture on sanitary sewer systems.
• Predicting geomorphologic changes, such as erosion or sedimentation.
• Assessing the impacts of natural and anthropogenic environmental change on water resources.
• Assessing contaminant transport risk and establishing environmental policy guidelines.
• Estimating the water resource potential of river basins.

History[edit]

Hydrology has been a subject of investigation and engineering for millennia. For example, about 4000 BC the Nile was dammed to improve agricultural productivity of previously barren lands. Mesopotamian towns were protected from flooding with high earthen walls. Aqueducts were built by the Greeks and Ancient Romans, while the history of China shows they built irrigation and flood control works. The ancient Sinhalese used hydrology to build complex irrigation works in Sri Lanka, also known for invention of the Valve Pit which allowed construction of large reservoirs, anicuts and canals which still function.

Marcus Vitruvius, in the first century BC, described a philosophical theory of the hydrologic cycle, in which precipitation falling in the mountains infiltrated the Earth's surface and led to streams and springs in the lowlands.^{[citation needed]} With adoption of a more scientific approach, Leonardo da Vinci and Bernard Palissy independently reached an accurate representation of the hydrologic cycle. It was not until the 17th century that hydrologic variables began to be quantified.

Pioneers of the modern science of hydrology include Pierre Perrault, Edme Mariotte and Edmund Halley. By measuring rainfall, runoff, and drainage area, Perrault showed that rainfall was sufficient to account for flow of the Seine. Marriotte combined velocity and river cross-section measurements to obtain discharge, again in the Seine. Halley showed that the evaporation from the Mediterranean Sea was sufficient to account for the outflow of rivers flowing into the sea.^[2]

Advances in the 18th century included the Bernoulli piezometer and Bernoulli's equation, by Daniel Bernoulli, and the Pitot tube, by Henri Pitot. The 19th century saw development in groundwater hydrology, including Darcy's law, the Dupuit-Thiem well formula, and Hagen-Poiseuille's capillary flow equation.

Rational analyses began to replace empiricism in the 20th century, while governmental agencies began their own hydrological research programs. Of particular importance were Leroy Sherman's unit hydrograph, the infiltration theory of Robert E. Horton, and C.V. Theis's aquifer test/equation describing well hydraulics.

Since the 1950s, hydrology has been approached with a more theoretical basis than in the past, facilitated by advances in the physical understanding of hydrological processes and by the advent of computers and especially geographic information systems (GIS). (See also GIS and hydrology)

Themes[edit]

The central theme of hydrology is that water circulates throughout the Earth through different pathways and at different rates. The most vivid image of this is in the evaporation of water from the ocean, which forms clouds. These clouds drift over the land and produce rain. The rainwater flows into lakes, rivers, or aquifers. The water in lakes, rivers, and aquifers then either evaporates back to the atmosphere or eventually flows back to the ocean, completing a cycle. Water changes its state of being several times throughout this cycle.

The areas of research within hydrology concern the movement of water between its various states, or within a given state, or simply quantifying the amounts in these states in a given region. Parts of hydrology concern developing methods for directly measuring these flows or amounts of water, while others concern modelling these processes either for scientific knowledge or for making prediction in practical applications.

Groundwater[edit]

Ground water is water beneath Earth's surface, often pumped for drinking water.^[1] Groundwater hydrology (hydrogeology) considers quantifying groundwater flow and solute transport.^[3] Problems in describing the saturated zone include the characterization of aquifers in terms of flow direction, groundwater pressure and, by inference, groundwater depth (see: aquifer test). Measurements here can be made using a piezometer. Aquifers are also described in terms of hydraulic conductivity, storativity and transmissivity. There are a number of geophysical methods^[4] for characterising aquifers. There are also problems in characterising the vadose zone (unsaturated zone).^[5]

Infiltration[edit]

Infiltration is the process by which water enters the soil. Some of the water is absorbed, and the rest percolates down to the water table. The infiltration capacity, the maximum rate at which the soil can absorb water, depends on several factors. The layer that is already saturated provides a resistance that is proportional to its thickness, while that plus the depth of water above the soil provides the driving force (hydraulic head). Dry soil can allow rapid infiltration by capillary action; this force diminishes as the soil becomes wet. Compaction reduces the porosity and the pore sizes. Surface cover increases capacity by retarding runoff, reducing compaction and other processes. Higher temperatures reduce viscosity, increasing infiltration.^{[6]:250–275}

Soil moisture[edit]

Soil moisture can be measured in various ways; by capacitance probe, time domain reflectometer or Tensiometer. Other methods include solute sampling and geophysical methods.

Surface water flow[edit]

Hydrology considers quantifying surface water flow and solute transport, although the treatment of flows in large rivers is sometimes considered as a distinct topic of hydraulics or hydrodynamics. Surface water flow can include flow both in recognizable river channels and otherwise. Methods for measuring flow once water has reached a river include the stream gauge (see: discharge), and tracer techniques. Other topics include chemical transport as part of surface water, sediment transport and erosion.

One of the important areas of hydrology is the interchange between rivers and aquifers. Groundwater/surface water interactions in streams and aquifers can be complex and the direction of net water flux (into surface water or into the aquifer) may vary spatially along a stream channel and over time at any particular location, depending on the relationship between stream stage and groundwater levels.

Precipitation and evaporation[edit]

In some considerations, hydrology is thought of as starting at the land-atmosphere boundary^{[citation needed]} and so it is important to have adequate knowledge of both precipitation and evaporation. Precipitation can be measured in various ways: disdrometer for precipitation characteristics at a fine time scale; radar for cloud properties, rain rate estimation, hail and snow detection; rain gauge for routine accurate measurements of rain and snowfall; satellite for rainy area identification, rain rate estimation, land-cover/land-use, and soil moisture, for example.

Evaporation is an important part of the water cycle. It is partly affected by humidity, which can be measured by a sling psychrometer. It is also affected by the presence of snow, hail and ice and can relate to dew, mist and fog. Hydrology considers evaporation of various forms: from water surfaces; as transpirationfrom plant surfaces in natural and agronomic ecosystems. A direct measurement of evaporation can be obtained using Simon's evaporation pan.

Detailed studies of evaporation involve boundary layer considerations as well as momentum, heat flux and energy budgets.

Remote sensing[edit]

Remote sensing of hydrologic processes can provide information on locations where in situ sensors may be unavailable or sparse. It also enables observations over large spatial extents. Many of the variables constituting the terrestrial water balance, for example surface water storage, soil moisture, precipitation, evapotranspiration, and snow and ice, are measurable using remote sensing at various spatial-temporal resolutions and accuracies.^[7] Sources of remote sensing include land-based sensors, airborne sensors and satellite sensors which can capture microwave, thermal and near-infrared data or use lidar, for example.

Water quality[edit]

In hydrology, studies of water quality concern organic and inorganic compounds, and both dissolved and sediment material. In addition, water quality is affected by the interaction of dissolved oxygen with organic material and various chemical transformations that may take place. Measurements of water quality may involve either in-situ methods, in which analyses take place on-site, often automatically, and laboratory-based analyses and may include microbiological analysis.

Integrating measurement and modelling[edit]

• Budget analyses
• Parameter estimation
• Scaling in time and space
• Quality control of data – see for example Double mass analysis

Prediction[edit]

Observations of hydrologic processes are used to make predictions of the future behaviour of hydrologic systems (water flow, water quality). One of the major current concerns in hydrologic research is 'Prediction in Ungauged Basins' (PUB), i.e. in basins where no or only very few data exist.

Statistical hydrology[edit]

By analyzing the statistical properties of hydrologic records, such as rainfall or river flow, hydrologists can estimate future hydrologic phenomena. When making assessments of how often relatively rare events will occur, analyses are made in terms of the return period of such events. Other quantities of interest include the average flow in a river, in a year or by season.

These estimates are important for engineers and economists so that proper risk analysis can be performed to influence investment decisions in future infrastructure and to determine the yield reliability characteristics of water supply systems. Statistical information is utilized to formulate operating rules for large dams forming part of systems which include agricultural, industrial and residential demands.

Modeling[edit]

Hydrological models are simplified, conceptual representations of a part of the hydrologic cycle. They are primarily used for hydrological prediction and for understanding hydrological processes, within the general field of scientific modeling. Two major types of hydrological models can be distinguished:^{[citation needed]}

• Models based on data. These models are black box systems, using mathematical and statistical concepts to link a certain input (for instance rainfall) to the model output (for instance runoff). Commonly used techniques are regression, transfer functions, and system identification. The simplest of these models may be linear models, but it is common to deploy non-linear components to represent some general aspects of a catchment's response without going deeply into the real physical processes involved. An example of such an aspect is the well-known behavior that a catchment will respond much more quickly and strongly when it is already wet than when it is dry.
• Models based on process descriptions. These models try to represent the physical processes observed in the real world. Typically, such models contain representations of surface runoff, subsurface flow, evapotranspiration, and channel flow, but they can be far more complicated. These models are known as deterministic hydrology models. Deterministic hydrology models can be subdivided into single-event models and continuous simulation models.

Recent research in hydrological modeling tries to have a more global approach to the understanding of the behavior of hydrologic systems to make better predictions and to face the major challenges in water resources management.

Transport[edit]

Water movement is a significant means by which other material, such as soil, gravel, boulders or pollutants, are transported from place to place. Initial input to receiving waters may arise from a point source discharge or a line source or area source, such as surface runoff. Since the 1960s rather complex mathematical models have been developed, facilitated by the availability of high speed computers. The most common pollutant classes analyzed are nutrients, pesticides, total dissolved solids and sediment.

Organizations[edit]

Intergovernmental organizations[edit]

• International Hydrological Programme (IHP)^[8]

International research bodies[edit]

• International Water Management Institute (IWMI)^[9]
• UN-IHE Delft Institute for Water Education^[10]

National research bodies[edit]

• Centre for Ecology and Hydrology – UK^[11]
• Centre for Water Science, Cranfield University, UK^[12]
• eawag – aquatic research, ETH Zürich, Switzerland^[13]
• Institute of Hydrology, Albert-Ludwigs-University of Freiburg, Germany^[14]
• United States Geological Survey – Water Resources of the United States^[15]
• NOAA's National Weather Service – Office of Hydrologic Development, USA^[16]
• US Army Corps of Engineers Hydrologic Engineering Center, USA^[17]
• Hydrologic Research Center, USA^[18]
• NOAA Economics and Social Sciences, USA^[19]
• University of Oklahoma Center for Natural Hazards and Disasters Research, USA^[20]
• National Hydrology Research Centre, Canada^[21]
• National Institute of Hydrology, India^[22]

National and international societies[edit]

• American Institute of Hydrology (AIH)^[23]
• Geological Society of America (GSA) – Hydrogeology Division^[24]
• American Geophysical Union (AGU) – Hydrology Section^[25]
• National Ground Water Association (NGWA)^[26]
• American Water Resources Association^[27]
• Consortium of Universities for the Advancement of Hydrologic Science, Inc. (CUAHSI)^[28]
• International Association of Hydrological Sciences (IAHS)^[29][30]
• Statistics in Hydrology Working Group (subgroup of IAHS)^[31]
• German Hydrological Society (DHG: Deutsche Hydrologische Gesellschaft)^[32]
• Italian Hydrological Society (SII-IHS) – http://www.sii-ihs.it
• Nordic Association for Hydrology^[33]
• British Hydrological Society^[34]
• Russian Geographical Society (Moscow Center) – Hydrology Commission^[35]
• International Association for Environmental Hydrology^[36]
• International Association of Hydrogeologists^[37]
• Society of Hydrologists and Meteorologists - Nepal^[38]

Basin- and catchment-wide overviews[edit]

• Connected Waters Initiative, University of New South Wales^[39] – Investigating and raising awareness of groundwater and water resource issues in Australia
• Murray Darling Basin Initiative, Department of Environment and Heritage, Australia^[40]

Research journals[edit]

• Hydrological Processes, ISSN1099-1085 (electronic) 0885-6087 (paper), John Wiley & Sons
• Hydrology Research, ISSN0029-1277, IWA Publishing (formerly Nordic Hydrology)
• Journal of Hydroinformatics, ISSN1464-7141, IWA Publishing
• Journal of Hydrologic Engineering, ISSN0733-9496, ASCE Publication
• Hydrological Sciences Journal - Journal of the International Association of Hydrological Sciences(IAHS)ISSN0262-6667 (Print), ISSN2150-3435 (Online)

See also[edit]

• Green Kenue a software tool for hydrologic modellers
• WEAP (Water Evaluation And Planning) software to model catchment hydrology from climate and land use data

Other water-related fields

• Oceanography is the more general study of water in the oceans and estuaries.
• Meteorology is the more general study of the atmosphere and of weather, including precipitation as snow and rainfall.
• Limnology is the study of lakes, rivers and wetlands ecosystems. It covers the biological, chemical, physical, geological, and other attributes of all inland waters (running and standing waters, both fresh and saline, natural or man-made).^[41]
• Water resources are sources of water that are useful or potentially useful. Hydrology studies the availability of those resources, but usually not their uses.

References[edit]

1. ^ ^abc'What is hydrology and what do hydrologists do?'. USA.gov. U.S. Geological Survey. Retrieved 7 October 2015.
2. ^Biswat, Asit K. 'Edmond Halley, F.S.R., Hydrologist Extraordinary'. JSTOR. Royal Society Publishing.
3. ^Graf, T.; Simmons, C. T. (February 2009). 'Variable-density groundwater flow and solute transport in fractured rock: Applicability of the Tang et al. [1981] analytical solution'. Water Resources Research. 45 (2): W02425. doi:10.1029/2008WR007278.
4. ^Vereecken, H.; Kemna, A.; Münch, H. M.; Tillmann, A.; Verweerd, A. (2006). 'Aquifer Characterization by Geophysical Methods'. Encyclopedia of Hydrological Sciences. John Wiley & Sons. doi:10.1002/0470848944.hsa154b. ISBN0-471-49103-9.
5. ^Wilson, L. Gray; Everett, Lorne G.; Cullen, Stephen J. (1994). Handbook of Vadose Zone Characterization & Monitoring. CRC Press. ISBN978-0-87371-610-9.
6. ^Reddy, P. Jaya Rami (2007). A textbook of hydrology (Reprint. ed.). New Delhi: Laxmi Publ. ISBN9788170080992.
7. ^Tang, Q.; Gao, H.; Lu, H.; Lettenmaier, D. P. (6 October 2009). 'Remote sensing: hydrology'. Progress in Physical Geography. 33 (4): 490–509. doi:10.1177/0309133309346650.
8. ^'International Hydrological Programme (IHP)'. IHP. Retrieved 8 June 2013.
9. ^'International Water Management Institute (IWMI)'. IWMI. Retrieved 8 March 2013.
10. ^'IHE Delft Institute for Water Education'. UNIESCO-IHE. Archived from the original on 14 March 2013.
11. ^'CEH Website'. Centre for Ecology & Hydrology. Retrieved 8 March 2013.
12. ^'Cranfield Water Science Institute'. Cranfield University. Retrieved 8 March 2013.
13. ^'Eawag aquatic research'. Swiss Federal Institute of Aquatic Science and Technology. 25 January 2012. Retrieved 8 March 2013.
14. ^'Professur für Hydrologie'. University of Freiburg. 23 February 2010. Retrieved 8 March 2013.
15. ^'Water Resources of the United States'. USGS. 4 October 2011. Retrieved 8 March 2013.
16. ^'Office of Hydrologic Development'. National Weather Service. NOAA. 28 October 2011. Retrieved 8 March 2013.
17. ^'Hydrologic Engineering Center'. US Army Corps of Engineers. Retrieved 8 March 2013.
18. ^'Hydrologic Research Center'. Hydrologic Research Center. Retrieved 8 March 2013.
19. ^'NOAA Economics and Social Sciences'. NOAA Office of Program Planning and Integration. Archived from the original on 25 July 2011. Retrieved 8 March 2013.
20. ^'Center for Natural Hazard and Disasters Research'. University of Oklahoma. 17 June 2008. Archived from the original on 24 May 2013. Retrieved 8 March 2013.
21. ^'National Hydrology Research Centre (Saskatoon, SK)'. Environmental Science Centres. Environment Canada. Retrieved 8 March 2013.
22. ^'National Institute of Hydrology (Roorkee), India'. NIH Roorkee. Archived from the original on 19 September 2000. Retrieved 1 August 2015.
23. ^'American Institute of Hydrology'.
24. ^'Hydrogeology Division'. The Geological Society of America. 10 September 2011. Retrieved 8 March 2013.
25. ^'Welcome to AGU's Hydrology (H) Section'. American Geophysical Union. Retrieved 8 March 2013.
26. ^'National Ground Water Association'. Retrieved 8 March 2013.
27. ^'American Water Resources Association'. 2 January 2012. Retrieved 8 March 2013.
28. ^'CUAHSI'. Retrieved 8 March 2013.
29. ^'International Association of Hydrological Sciences (IAHS)'. Associations. International Union of Geodesy and Geophysics. 1 December 2008. Retrieved 8 March 2013.
30. ^'International Association of Hydrological Sciences'. Retrieved 8 March 2013.
31. ^'International Commission on Statistical Hydrology'. STAHY. Retrieved 8 March 2013.
32. ^Deutsche Hydrologische Gesellschaft, accessed 2 September 2013
33. ^Nordic Association for Hydrology, accessed 2 September 2013
34. ^'The British Hydrological Society'. Retrieved 8 March 2013.
35. ^'{title}' Гидрологическая комиссия [Hydrological Commission] (in Russian). Russian Geographical Society. Archived from the original on 26 August 2013. Retrieved 8 March 2013.
36. ^'Hydroweb'. The International Association for Environmental Hydrology. Retrieved 8 March 2013.
37. ^'International Association of Hydrogeologists'. Retrieved 19 June 2014.
38. ^'Society of Hydrologists and Meteorologists'. Society of Hydrologists and Meteorologists. Retrieved 12 June 2017.
39. ^'Connected Waters Initiative (CWI)'. University of New South Wales. Retrieved 8 March 2013.
40. ^'Integrated Water Resource Management in Australia: Case studies – Murray-Darling Basin initiative'. Australian Government, Department of the Environment. Australian Government. Retrieved 19 June 2014.
41. ^Wetzel, R.G. (2001) Limnology: Lake and River Ecosystems, 3rd ed. Academic Press. ISBN0-12-744760-1

Further reading[edit]

• Anderson, Malcolm G.; McDonnell, Jeffrey J., eds. (2005). Encyclopedia of hydrological sciences. Hoboken, NJ: Wiley. ISBN0-471-49103-9.
• Hendriks, Martin R. (2010). Introduction to physical hydrology. Oxford: Oxford University Press. ISBN978-0-19-929684-2.
• Hornberger, George M.; Wiberg, Patricia L.; Raffensperger, Jeffrey P.; D'Odorico, Paolo P. (2014). Elements of physical hydrology (2nd ed.). Baltimore, Md.: Johns Hopkins University Press. ISBN9781421413730.
• Maidment, David R., ed. (1993). Handbook of hydrology. New York: McGraw-Hill. ISBN0-07-039732-5.
• McCuen, Richard H. (2005). Hydrologic analysis and design (3rd ed.). Upper Saddle River, N.J.: Pearson-Prentice Hall. ISBN0-13-142424-6.
• Viessman, Jr., Warren; Gary L. Lewis (2003). Introduction to hydrology (5th ed.). Upper Saddle River, N.J.: Pearson Education. ISBN0-673-99337-X.

External links[edit]

LEVEL 1 CERTIFICATION

About MovNat & Natural Movement®

MovNat is a fitness and physical education system based on the full range of natural human movement skills. The Movnat system trains physical competence for practical performance. Based on effective, efficient, and adaptive movement modalities.

Level 1 Certification

The MovNat Level 1 (MCT) Certification Trainer Certificate Course is an introductory course on methodology, concepts, background and movements. The program includes lectures on: Natural Movement concepts and modalities, Essential movements, coaching & teaching strategies, and dietary & lifestyle recommendations.

The movement training include small group sessions in which attendees are instructed & evaluated in MovNat movement techniques. These small training sessions are essential for engaging in dialogue and critique of movements. Methods are discussed for optimizing both an individuals movements and how to instruct others.

Best practices are discussed at the end of the workshop, as well as strategies for teaching Natural Movement in multiple environments and scaling for any fitness level.

2.5 day Certification vs 2 day Introduction workshop

Our level 1 certification workshops mix 2 types of participants: the participants to the 2 day workshop (training only) and those who attend the 2.5 day certification workshop as candidates. Here is the list of advantages only candidates to the certification will benefit:

• An extra half day of theory and practice, with additional testing at end of third day.
• Access to the certification manual and training video library upon registration (allowing you to learn and practice before the workshop).
• Examination of theory, personal skills and coaching abilities at the end of the workshop.
• Access to the private MCT forum and Facebook page (upon passing the certification)
• Being listed in our MCT locator (upon passing the certification) on movnat.com
• (limited) Right to use the “MovNat Natural Movement Certified Trainer” mention and logo on your business cards, website or printed material.

PURPOSE

The Level 1 Certification Course is an introduction to MovNat’s modality and foundational movements. The course includes lecture, movement instruction, as well as written and physical evaluation.

Mar 21, 2019 - Breakthrough BeatLock engine is a great feature of Virtual DJ pro 7 crack that keep your songs in tune. Breakthrough BeatLock engine allows. May 20, 2019 - Virtual DJ Pro 2019 Crack is the audio and video mixing software with its breakthrough BeatLock engine, songs will stay in beat always, and the DJ works their mixes incredibly faster than they ever could. One new exclusive feature of Virtual DJ Pro Serial Key is the“sandbox that. 08-Jun-2019- Virtual DJ Pro 7 Crack Full Version Free Download. Crack virtual dj pro 7.

As an introductory level education on Natural Movement. It is designed to:

• Provide trainers with a better knowledge and understanding to continue their own Natural Movement practice.
• Provide the foundation & skills necessary to being teaching Natural Movement to others.

Potential MCT’s should view the Level I Certification Course as the beginning of the journey. The course is not designed to be a comprehensive or all-encompassing education in Natural Movement. Rather it provides a basic certification to begin teaching, as well as the foundation to continue one’s own movement practice.

CERTIFICATION BENEFITS

• Speak and explain the core principles of Natural Movement
• Understand essential movement concepts such as body-weight shift, point of support, etc
• Be able to evaluate, verbalize, and correct movement technique
• Teach Natural Movement safely and effectively.

EVALUATION

The evaluation has three components:

• Movement technique
• Coaching ability
• Written Test Evaluation

Instructors will evaluate your movement technique throughout the weekend. The complete list of movements that will be covered in the Level 1 Certification is listed on this page. As soon as participants register, they will be given access to the video library which contains a full series of instructional videos for each movement. Learning and practicing these movements is essential for success at MovNat Certification.

The coaching ability is evaluated through video sample at the Level 1 Certification. Based on a test scenario, your ability to identity movement inefficiency and effectively correct movement patterns will be evaluated. Trainers will be expected to be able to verbalize and demonstrate proper technique on all Level 1 movements.

After registration, participants will be sent the MovNat Trainer Manual. Studying this manual is essential to passing the written evaluation.

The written evaluation has been designed to guarantee a competency and fluency with the concepts and ideas of Natural Movement. As a trainer, it is essential to be able to communicate these concepts to the public. The test contains 25 multiple-choice questions. A passing score of 80% or better is required. All of the test questions come directly from the lectures, video library, and the MovNat Trainer Manual.

SAMPLE TEST QUESTIONS:

Q -What are the 4 grips?
A. Crossed fingers grip, Wrist grip, Gable grip, S-grip.
B. Wrist grip, V-grip, Crossed fingers grip, Plough grip.
C. Gable grip, V-grip, Plough grip, Crossed fingers grip.
D. S-grip, Crossed fingers grip, Swing grip, Wrist grip.

Q – The following description is about which technique?
This technique is primarily used after a depth jump (or a jump from height). It is useful in dispersing a significant amount of the impact forces throughout the entire kinetic chain, rather than leaving them localized primarily in the lower body.
A. Squat Landing
B. Slap Landing
C. Swing Landing
D. Rotational Landing

FAILURE

Natural English Moving 1 Pdf Free

Failure in any area of evaluation will result in no certification being issued to participant. However, logistics permitting, the candidates who fail some of the tests might be allowed to re-take the tests during the same week-end.

ELIGIBILITY

Candidates must have some basic knowledge of human anatomy & physiology and/or kinesiology.

They also must be:

• 18 years old
• CPR/AED certified.

Natural English Moving 1 Pdf Converter

NON-DISCRIMINATION

Natural Movement is for everyone. MovNat endorses the principles of equal opportunity – the MCT program is available to all participants regardless of age, race, religion, gender, national origin, veteran status, sexual preference or orientation.

LANGUAGE

The default language for the Level 1 Course is English. However, depending on the local logistics, some workshops might have a local MovNat Trainer who could translate some lectures. The written exam is always in English, though

LIST OF TECHNIQUES COVERED BY THE LEVEL 1 CERTIFICATION

General running technique
Lateral running
General balancing technique
Pivot-reverse™
Cross-reverse™
General landing
Slap landing
Leg swing™ jump
Broad jump
Vertical jump
Depth jump
Tripod vault
Split vault
Single-handed side vault
Double-handed side vault
Knee-hand crawl™
Foot-hand crawl™
Push-pull crawl™
Inverted crawl
Shoulder Crawl
Tap-swing
Tuck-swing
Swing Brake
Forward Swing traverse
Side Swing traverse™
Power traverse™
Hook traverse™
Rotational swing throw
Chest throw
Rotational swing catch
Chest catch
Deadlift
Lapping
Shouldering
Push Press
Waist Carry
Chest Carry

PAYMENT DETAILS

All participants are required to register for the Level 1 Certificate at MovNat.com using the link for the specific event. The link will take the participant to a third-party registration system (EventBee) for registration and payment. Arrangements to pay by check or other method are permissible, please contact MovNat at contact@movnat.com to obtain specific details.

To inquire about the possibility of a payment plan please contact vic@movnat.com

USE OF MOVNAT CERTIFICATE AND TRADEMARK

– IMPORTANT INFORMATION –

• Both “MovNat” and “Natural Movement” are USPTO registered trademarks. MovNat LLC owns the exclusive right of use in commerce of both trademarks. The use in commerce of both the MovNat and Natural Movement trademarks by MovNat Certified Trainers is subject to specific limitations (see below).
• For information regarding becoming a MovNat/Natural Movement affiliate, please contact us.

MovNat Certified Trainer (MCT) Privileges Prerequisite: MovNat Certified
Trainer – Natural Movement Level 1

MOVNAT CERTIFIED TRAINER RIGHTS:

• List the trainer certification on personal business materials, as follows: Your name, MovNat Certified Trainer (or MovNat Natural Movement Trainer)
• Designate that you are a “MovNat Certified Trainer” or “MovNat Natural Movement Trainer” on your website, business cards, and all promotional materials.
• Use the MovNat Certified Trainer logo which will be available upon completion of the course.
• Use the MovNat Certified Trainer logo in the certified trainer’s business materials.*
• We recommend wearing MovNat or “MovNat Natural Movement Fitness” on your local branded attire when teaching MovNat.
• Have access to the private MCT Forum hosted on www.movnat.com

LIMITATIONS:

• Cannot use the MovNat or Natural Movement trademarks, names, slogans, artwork, photos, videos or copy content from the MovNat website in any other business or promotional manner.
• Linking to content and videos on the MovNat, LLC site is acceptable.
• Cannot use the MovNat or Natural Movement trademark and name in your business name, videos, web address, or facility name.
• The MovNat Certified Trainer title does not allow for the use of MovNat and Natural Movement trademarks, names, slogans, artwork, photos, or content from the MovNat website in any other business or promotional manner.
• Any MovNat videos you develop for your website must be high-quality, professional and approved by MovNat, LLC

Please contact us at contact@movnat.com with any additional questions you have regarding MovNat Certification.