![]() Each member of the team must read, understand and execute the Waiver as well as fill out all proper registration forms. Persons under the age of sixteen (16) years of age at the time of the event are ineligible. Each team must consist of at least one (1) person 18 years of age or older. Hunters shall register in teams of two (2) persons. The Professional Hunter understands and agrees that his/her registration fee and any and all prizes or money obtained through Quest Hunt shall be forfeited. In the event the Quest Hunt becomes aware that a Professional Hunter has registered with Quest Hunt, the Professional Hunter shall be immediately and permanently disqualified from Quest Hunt competitions and events. For the purposes of this agreement, a professional hunter is defined as a person who receives any income from hunting deer and/or a person who receives any income from creating footage, whether in video, audio or other electronic forms, of deer hunting. Any person who is a professional hunter is ineligible for Quest Hunt competition. The Participation Agreement and the Waiver, as well as any and all updates and changes thereto, shall be available at NO PROFESSIONAL HUNTER. It is the sole responsibility of each registered hunter to read and understand the Participation Agreement and the Complete Waiver and Release of Liability Agreement to Hold Harmless and Assumption of Risk (“Waiver”). Quest Hunt reserves the right to amend and/or modify this Participation Agreement. Quest Hunt shall have exclusive authority to interpret and enforce the terms of the Participation Agreement. Such surveys would permit detailed analysis of controls of sedimentological connectivity across badlands and their influence on channel networks and catchment sediment budgets.This Participation Agreement shall be used solely for the tournaments and events produced, sponsored or coordinated by Quest Hunt Co., LLC (“Quest Hunt”). Although the approach outlined in this paper was only applied to a relatively small area, with careful survey design and application of new survey technology, it could readily be upscaled to cover entire badland systems. ![]() Overall, the results indicate that coupling of appropriately-scaled spatial and temporal data is critical to understand topographic changes and their drivers on badlands. Erosion proved to be dominant on slopes higher than 100%. At the annual scale the effect of aspect in the sign of the topographic change was removed and slope becomes more important. Our observations suggest that longer-term studies may underestimate the importance of surface roughness as a control on badland geomorphology. Although these patterns could be also affected by swell-shrink processes, surface roughness was more important at controlling badland geomorphological processes at the event-scale than the annual scale. Net topographic change at the event scale varied from − 1.8 to 1.4 cm. Aspect, surface roughness and slope were significant predictors of topographic change, although the sign and magnitude of the change differed at the event scale. annual net change at around − 6 cm yr − 1). Our results show a clear erosional pattern for most of the badland at the annual scale (i.e. Data analyses were conducted on two temporal scales: (a) five rainfall events and (b) three long term (spaced over an annual cycle) scales. In this paper we demonstrate how reliable estimates of topographic variables and temporal change can be derived for badlands by repeat Terrestrial Laser Scanning (TLS) surveys undertaken at multiple temporal (event to annual) scales.Ī total of seven TLS-surveys were obtained in an experimental sub-humid badland located in the Central Pyrenees. Recent developments in survey instrumentation provide the opportunity to build high-resolution topographic models over multiple spatial scales at sub-centimeter accuracy. Erosion rates from badlands have been widely estimated by discrete observations of topographic change measured by erosion pins or profile meters. Badland surfaces experience high erosion rates that may have a direct and marked influence on river channel networks and catchment scale sediment budgets. ![]() Badlands are highly erodible landscapes with sparse vegetation and rapid runoff responses.
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