Researching the Dam

August 1, 2025
Author: Michael Marlatt, OLS, CLS (Ret.)

When discussing land surveyors’ research on the water-side boundaries of riparian land parcels, it is important to distinguish between the influence of artificial or unnatural processes or activities, usually caused by human activity, as distinct from the natural processes, that can and do occur at the water’s edge. Both types of processes or activities may influence the legal position of a riparian parcel boundary, either in agreement or in disagreement with the physical location of the water’s edge. Research on these processes is as important as the research on the original survey and other documentary records initially creating the riparian boundary.

This paper primarily focuses on “damming”, the process for artificially changing the natural water level of a lake, pond, river, creek, or any waterbody or watercourse with a distinct title interest or geographic designation from the abutting uplands. The existence and possible impacts of a damming structure on a waterbody or watercourse that bounds a parcel of land to be surveyed raise questions and potential ambiguities that require thorough research. It is argued such research should include a comprehensive examination of evidence and facts relating to the damming structure and its operations.

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No Man is an Island

August 4, 2025
Author: Tom Bunker OLS, (Ret.)

In No Man is an Island, Tom Bunker takes us on a fascinating journey into the world of islands—both the kind you see on a map and the kind that live in the fine details of a surveyor’s work. He shows us that islands are never just “lumps of land in water.” They hold history, shifting boundaries, and stories of change over time. Whether you’re a surveyor, a history enthusiast, or simply curious about how land and water shape each other, Tom’s article will open your eyes to details you might never have noticed. It’s a thoughtful reminder that no island—and no person—truly stands alone. lands as either Canada West/Upper Canada, or Canada East/Lower Canada, lands.

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Albert Pellew Salter's Exploration, Base, Meridian and Range Line Survey 1856 - 1858

March 30, 2025
Author: Michael Marlatt, OLS, CLS (Ret.)

The colony of Quebec, under British rule following the Seven Years’ War, was divided
into the Provinces of Upper and Lower Canada pursuant to the initial directions set out by the 24 August 1791 Order of King George III, with the advice of his Privy Council. The proposed division was carried into effect by the enactment of Imperial Act, 31 George III, c. 31, now known as the Constitution Act, 1791, which repealed certain portions of the Quebec Act, 1774 and provided a new constitution for the government, organization, and administration of the two new provinces.


Subsequently, by Imperial Statute 3-4 Victoria, c. 35: An Act to re-unite the Provinces of
Upper and Lower Canada, and for the Government of Canada, enacted on 23 July 1840 and proclaimed on 10 February 1841, also known as the Act of Union, the two Provinces were reunited to become the Province of Canada. However, the two former geographic entities continued to be governed and administered separately as Canada West and Canada East sections of the province according to the Upper and Lower Canada divisions, including formal and informal, and interchangeable, use of the four names. More specifically, the Crown Lands Department for the Province of Canada continued to administer Provincial lands as either Canada West/Upper Canada, or Canada East/Lower Canada, lands.

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Illustrating Artificial and Natural Physical Features on Plans of Survey

October 1, 2024
Author: Survey Review Department and Professional Standards Committee

AOLS receives inquiries regarding the illustration and dimensioning of artificial and natural physical features on survey plans. Plans are not always clear as to where ties are taken (centre of fence, edge of fence, at top of retaining wall, at base of retaining wall, etc.). These inquiries are from both OLS and the public. In the absence of any recommended best practice, the AOLS Professional Standards Committee (PSC) and AOLS Survey Review Department (SRD) have prepared this paper.

As there are a very large number of different artificial (buildings, fences, walls, walkways, driveways, etc.) and an equally large number of natural (shorelines, embankments, swamps, trees, land masses, etc.) features, this document will only detail a representative sample but hopefully provide guidance for the illustration of all. There are three considerations –illustration & labelling, dimensions & ties and precision & accuracy.

The underlying principals are clarity and consistency. The illustration method and/or plan notes should enable users of the plan to determine the nature and location of the feature.

This paper DOES NOT discuss or make comment on artificial and natural physical features as EVIDENCE of interests in or usage of land. This paper does not provide any guidance on what part of a fence or other structure should be used to define a boundary nor does this paper provide any guidance on what constitutes a ‘high water mark’ or ‘water’s edge’. These complex issues require specific research of the individual circumstance and through research and knowledge of relevant common and statute law.

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OLS Project Oversight

August 23, 2024
Author: Survey Review Department and Professional Standards Committee

Section 35, Subsection 6 of Ontario Regulation 1026 (Surveyors Act) requires survey plans or other deliverables to be prepared under the supervision of an OLS. There are several other sections of Regulation 1026 and 216/10 that specify requirements for OLS project supervision.

It is noted that these regulations apply to both licensed and registered OLS.

The practical need or the ‘level’ of oversight on a project varies with factors such as the:

  • type and complexity of project,
  • firm / surveyor experience with that type of project,
  • staff experience and knowledge,
  • work performed from ‘remote’ locations where the project surveyor is not in attendance (e.g. work from home, project surveyor and staff in separate offices, etc.),
  • project ‘risk factors’ – consequence, financial or otherwise, of error or delivery failure,
  • statutory or other legal requirements (Boundaries Act, Court Case, etc.),
  • ‘Quality Assurance’ processes within firm.

Surveyors and survey companies need to develop policies and process to meet these requirements and to help reduce errors arising from insufficient supervision.

To assist surveyors, the AOLS Survey Review Department and the AOLS Professional Standards Committee has prepared a document that outlines the regulations with suggestions on the ‘level’ of oversight required.

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A Tribute to Dr. J. Tuzo Wilson


July 19, 2024
Author: Vic Tyrer - Ontario Science Centre Staff Geographer (1978-199)

The recent announcement of the Ontario Science Centre's permanent closure has far reaching impacts, including the fate of the J. Tuzo Wilson Geodetic Monument.

Dr. J. Tuzo Wilson was the Ontario Science Centre's third Director General from 1974 to 1985. He passed away in 1993 at the age of 84. In tribute to Dr. Wilson, a new exhibit was unveiled in May of 2000 on the plaza leading to the newly renovated entrance of the Science Centre. In attendance that day was his wife, Isabel and daughters Patty and Susan. Since then millions of visitors have walked past this unique exhibit depicting the relentless travel of the North American tectonic plate.

The tribute to Dr. Wilson was a massive, corroded steel “spike” rising several meters above the plaza created by the Science Centre to commemorate Dr. Wilson for the revolutionary change he brought upon the world's understanding of how Earth's invisible interior works. That foundational understanding today explains both the slow and sudden geological events that command our attention.

While formally addressed as Dr. Wilson, Science Centre colleagues, scientific peers and family, then and now continue to think of him as Tuzo.

A plaque with Tuzo’s likeness and some text affixed to a wall in the Centre would not have sufficed.  Instead, a fitting tribute would distill his life’s work into its simplest expression, and in keeping with the Centre’s design philosophy meet a fundamental requirement. His science had to be accurately represented. It had to be the real thing, like the lunar rock sample in the Astronomy Hall. And, the exhibit had to depict science in a manner relevant to the Centre’s visitors. 

A geodetic monument was considered the appropriate way to represent Tuzo’s scientific career. A geodetic monument is a physical marker typically secured into bedrock or embedded in stable ground, in this case an architectural rendering of a giant spike anchored into the Centre’s concrete plaza. A reference point is selected on the monument to which measurements can be made so that coordinates can be determined in terms of latitude, longitude, and height.

To recognize the significance of Tuzo Wilson's role in creating a paradigm shift in how we understand the tectonic forces that shape our Earth, the Canadian Geodetic Survey (a Division of Natural Resources Canada) undertook a geodetic survey on July 7th and 8th 1997, after the concrete base of the monument was in place. A GPS receiver was set up over the geodetic reference point in the base of the monument and for 24 hours, from 12:56 p.m. on the 7th to 1:01 p.m. on the 8th, signals from dozens of orbiting GPS satellites were tracked. To ensure the highest degree of accuracy, a perimeter of 5 m was secured around the GPS station to keep curious visitors and vehicles from interfering with the satellite signals.

The coordinates of the geodetic reference point were then transcribed onto the steel spike and the distinctive monument secured in place above its reference point. Today, it’s common knowledge that, on average, the seemingly solid ground of the North American tectonic plate is moving from east to west at about 1 to 2 cm/year depending on location. More specifically, the J. Tuzo Wilson geodetic monument is moving westward at 1.6 cm/yr. Other common tectonic terms, popular with trivia games include the Pacific Ring of Fire, mid-ocean ridges, subduction zones and the San Andreas Fault. These planetary-scale phenomena were finally brought together in a unified theory by Tuzo Wilson in the early 1960s. That theory, called Plate Tectonics is his legacy.

Decades after the initial geodetic survey of Tuzo’s monument, thousands of geodetic reference points throughout the North American plate are now continuously monitored by GPS revealing new refinements in our understanding of plate motion. For example, we now know that the overall average motion of a plate differs from that along plate boundaries where plates collide and deform in different ways.

Tectonic plate movement and drying paint are equally dull to watch. So how to depict the cumulative drift of North America towards the west coast? This is the second unique feature of the geodetic monument found at the visitor’s feet. Visitors were asked to imagine that the steel spike was driven into the Earth’s mantle; an immovable fixed reference point which the North American plate then slowly grinds past under tectonic forces, leaving a gash of broken concrete in the spike’s wake.  The 1.4 m gash in the plaza floor trending towards the west represents the amount of plate motion over Tuzo’s life of 84 years.

Other comparisons of the accumulation of tectonic motion can be made. For example, Canada has drifted westward about 2.5 m since Confederation. Or about half a metre of plate motion has occurred since the survey was done twenty seven years ago.  And the during the life of the Ontario Science Centre, as generations have known it, a tectonic tear of about 1 m in length would have resulted.

What is to become of this tribute to a Canadian pioneer of Earth Science?  One thing is certain, if the J. Tuzo Wilson geodetic monument is moved even a few centimeters from its original position, this geodetic monument (CGS #973026) loses its accuracy. It becomes just an architectural reminder of the Ontario Science Centre’s past.

Perhaps Tuzo’s spike should be relocated to the Department of Earth Sciences at the University of Toronto where he served as its first professor in 1946. Or, sent to locations that are significant to his insight and research. Iceland would be fitting. It is above a mantle plume (hot spot), that coincides with where the North American and Eurasian plates diverge along the mid-Atlantic Ridge. Or submerged into one of the two active volcanoes (seamounts) off the west coast of Vancouver Island named in Tuzo’s honour.

For a compressive and engaging biography of Tuzo’s life, research and achievements look for the book “Tuzo: The Unlikely Revolutionary of Plate Tectonics” by Nick Eyles, published by the University of Toronto Press and available online and at most bookstores.

Coordinates as Evidence - Cadastral Surveying


June 21, 2024
Essay written by Paul Wyman, OLS, with contributions by Morgan Goadsby, OLS (MNRF), and Ron Berg, OLS (MTO)

This essay looks at the current and possible future uses of provincial/national geodetic coordinates both from the perspective of coordinates as measurements but also as the primary definition of a legal interest in property – essentially replacing the physical survey monument.

The primary focus of the essay is not to come to any conclusions on the future use of coordinates – it is the marketplace that will likely decide in any event. It is, however, already clear that surveyors are and will increasing provide provincial/national geodetic coordinates as one of their ‘deliverables’. The essay is the start of a discussion within AOLS on standards for coordinates created as part of cadastral surveys and in particular, the need to preserve their meta data as new coordinate systems are introduced in the next 5 years.

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Drone Mapping: How to Select a LiDAR System


January 5, 2024

Ahmed El-Rabbany, Ph.D., P.Eng.
Toronto Metropolitan University

Selecting a survey-grade LiDAR system for drone-based topographic mapping can be challenging, especially when the system’s data sheet is difficult to read and/or lacks critical information. To appropriately select a commercial drone LiDAR system, users should consider the characteristics of four different sensors, namely the LiDAR sensor itself, the GNSS system, the inertial measurement unit (IMU), and the RGB camera. In addition, the accompanying software and its capabilities, including strip adjustment, are critical elements to consider. As a plus, a mission planning software, perhaps from the same manufacturer, should also be considered.

Survey-grade LiDAR systems will typically integrate GNSS and IMU data, as the two complement each other. While GNSS provides the initialization and the corrections to the inertial system, the latter provides high rate data and bridges the GNSS gaps when the satellite signal is blocked or temporarily lost for a short period (a few 10s of seconds). Typically, GNSS will be a high-end multi-constellation, multi-frequency system! This, however, is not necessarily the case with the IMU. High-quality GNSS/IMU results in precise trajectory and orientation (heading, pitch, roll) of the drone (and consequently, the LiDAR system). As the drone orientation (AKA attitude) plays a critical role in the accuracy of the resulting LiDAR point cloud, and since the orientation is obtained essentially from the IMU, the quality of the IMU is critical. In fact, a poor-quality IMU not only affects the accuracy of point cloud coordinates, but also requires frequent on-the-job calibration, which decreases the productivity. The user should consult the data sheet (specifications) for information about the GNSS/IMU sensor quality as well as the positioning and attitude accuracy.

Two survey-grade drone LiDAR sensors are currently available on the market, namely mechanical spinning (single- and multi-beam) and solid state. High-end drone LiDAR sensors are typically single-beam mechanical spinning. Examples of these LiDAR sensors are CHCNav AlphaAir 10 and Riegl VUX-120. Multi-beam mechanical spinning LiDAR sensors tend to be more noisier than the single-beam counterpart. Examples of multi-beam spinning LiDAR sensors include the Hesai XT32M2X and the Velodyne Ultra Puck. Solid-state LiDAR sensors, on the other hand, are typically low-cost sensors. Examples of LiDAR systems that make use of solid-state LiDAR sensors include CHCNav AlphaAir 450, and DJI Zenmuse L1 and L2.

When selecting a LiDAR sensor, a number of factors must be considered. These include the sensor characteristics, sensor weight and cost, and the application. Among the important sensor characteristics are the maximum measuring range, its accuracy/precision and the corresponding measuring conditions (e.g., target reflectivity, measuring altitude, incident angle, ambient weather condition), the operating flight above-ground level (AGL), the laser beam footprint (or equivalently, beam diversion), the scan speed and rate, the number of returns (echoes), and the field of view (FOV). The maximum measuring range represents the maximum slant distance (not the altitude), which is typically given for a 20% target reflectivity [note: target reflectivity is a function of surface composition (materials), for example: snow and limestone are highly reflecting surfaces (about 80%); sand (about 60%); concrete (about 30-40%); asphalt (about 10-20%)]. Range uncertainty varies with target geometry and size, distance to target, scan incident angle, environmental condition (e.g. fog, dust, bright sunlight), and target reflectivity. Typical specifications will provide the maximum range for flat targets with size larger than the laser footprint, excellent atmospheric visibility condition, and perpendicular scan incident angle. However, it should be pointed out that the maximum range will be reduced if laser pulse hits more than one target, as the total laser transmitter power will be split. As well, the range uncertainly will be increased as the distance to target increases, under poor environmental conditions and lower target reflectivity. Furthermore, the range uncertainly will be increased if incident angle is not perpendicular–the larger the incident angle is, the larger the range uncertainly.

When comparing different systems, users must make sure that the comparison is performed under the same conditions! For example, some manufacturers provide range precision and accuracy at a 30 m or 50 m range, while other provide them at a 100 m or even 150 m. As the uncertainty increases with distance (altitude), a 1 cm precision at a 50 m altitude, for example, will be larger when it is estimated at a 100 m altitude and much larger when it is estimated at a 150 m altitude.

The maximum operating flight above-ground level (AGL) will always be smaller than the maximum measuring range of the LiDAR system. Typically, manufacturers will provide both of the maximum AGL and maximum measuring range of their LiDAR systems in the data sheet. As such, when comparing different systems, a user should consider both. Users should also take into consideration that the maximum drone flight altitude in Canada is limited to 400 feet, or 120 m (unless the pilot-in-command obtains a Special Flight Operation Certificate (SFOC) from Transport Canada).

An important element that must be considered when examining the laser beam footprint (or beam diversion) is how it is defined! In fact, the laser beam spreads out as it travels away from the LiDAR sensor. The angular measure of the diameter of the laser beam is called beam diversion. Additionally, the laser beam profile does not have sharp edges – i.e., the radiant energy falls off gradually away from the centre of the beam. Most laser beam profiles can be approximated using the so-called Gaussian function (i.e., falls off approximately exponentially). As such, there are three ways that are commonly used to define LiDAR beam footprint (beam diversion): (1) the footprint at 50% peak intensity, i.e., when the radiant energy falls off to 50% of the peak intensity (also known as full width at half maximum, FWHM); (2) the 1/e point (corresponds to 36.8% of peak intensity); and (3) the 1/e2 point (corresponds to 13.5% of peak intensity). To correctly compare LiDAR sensors, the same definition must be used. It should also be pointed out that the beam divergence (or footprint) given in the data sheet represents the one measured at a zero scan (incident) angle (i.e., in the vertical direction). As the scan incident angle increases, the footprint increases. For example, consider a flat terrain and a LiDAR system with the following specifications: max. range = 150 m, max. AGL = 90 m, FOV = 360°, footprint = 15*10 cm (at 50% peak intensity). For such a system, although the system’s FOV is 360°, the actual FOV at the maximum range and maximum AGL will be limited to 106°! In addition, the footprint at the edge of the actual FOV (i.e., at an incident angle of 53°) will be about 25*17 cm (at 50% peak intensity). If we consider the more realistic 1/e2 point, rather than the 50%, the beam footprint will be about 42*29 cm. In fact, because of the large footprint (and uncertainty) at the outer beams, it is typically recommended to limit the FOV to a maximum of 80° or 90°.

The importance of the laser footprint size is that the smaller the footprint is, the higher the precision of distance measurement and the finer the resolution of topographic details that can be obtained. In other words, a small laser beam footprint (i.e., a small beam divergence) results in a higher quality digital terrain model (DTM) of the project area. On the other hand, a LiDAR with a large footprint beam will typically result in a lower precision of distance measurement (laser energy spreads over a larger area on the ground, which increases the noise) and a coarser resolution of topographic details. The number of returns, or echoes, and scan speed are also critical, especially for areas with high vegetation. Typically, for a survey-grade LiDAR sensor, an emitted pulse will have no returns, one return, or multiple returns. The no-return situation occurs, for example, when the distance between the senor and the target exceeds the maximum range. The one-return case, on the other hand, occurs, for example, when the laser pulse hits the ground surface with no other targets in the way. In forests or areas with high vegetation, the laser pulse will hit different parts of the forest (e.g. branches, leaves) till it reaches the bare ground, or perhaps loses all of its energy before it reaches the bare ground. Each target hit will reflect a signal (a return) to the LiDAR sensor with a different strength (intensity), which plays an important role in classifying the different objects in the project area. A high-end LiDAR will have multiple returns, and the last return will define the bare ground to a high degree of probability. The AlphaAir 10 LiDAR, for example, has a very small beam divergence of 0.33 mrad (corresponding footprint is 3.3*3.3 cm) at a 100 m altitude (50% peak intensity) and can provide up to 8 returns (sensevillegeo.com). This means that the likelihood of hitting the bare ground is very high, even for high vegetated areas, and the resulting DTM will be of high resolution.

Scan speed, pulse repetition rate (PRR), scan point density and spatial point distribution (pattern) are critical elements that distinguish a LiDAR sensor from another! Scan speed represents the number of scan lines (AKA scans or swaths) per second, while PRR (AKA pulse repetition frequency) represents the number of laser pulses that the sensor emit per second. Scan line spacing on the ground is directly related to the scan speed and drone speed. For example, for the AlphAir 10 LiDAR, scan speed can be as high as 250 lines per second. For such a scan speed, the corresponding line spacing on the ground for a drone travelling at 10 m/sec would be 4 cm! PRR, on the other hand, is directly related to the number of measurements per second of the sensor – for a single return, the two are equal if no pulses are lost! Point density refers to the number of points (i.e., measurements) per square meter. Ideally, point density should be uniform (i.e., point-to-point distance is more or less constant) and as high as possible to ensure that we obtain an accurate and detailed DTM of the project area. Typically, however, LiDAR sensors have different scan mechanisms and may not necessarily have the same scan patterns! While the spatial point distribution of some sensors is unform, other sensors have different scan patterns, including sinusoidal, zig-zag, and elliptical. If the point density is very low, users should additionally consider the scan pattern when examining a LiDAR sensor. This is especially important when scanning an area with a substantial elevation difference (hilly terrain, open pit mine) or dense vegetation.

The PRR is typically used to define the proper drone flying height, drone speed, and point density during data acquisition. As the flying height increases, the energy of the arriving laser pulse becomes weaker to the extent that some LiDAR sensors would not be able to provide range measurements to low reflecting targets (e.g., 10%). Lowering the PRR increases the per-pulse energy, which in turn might help increase the flying altitude. However, a higher PRR allows for a faster drone speed while maintaining an appropriate point density. On the other hand, a low PRR means that we have to fly the drone at a lower speed to maintain a similar point density. This translates to a longer data acquisition time and an expensive project execution! The AlphaAir 10 LiDAR system, for example, has a high PRR of 500 kHz (500,000 measurement per seconds, single return) at an altitude of up to 120 m (maximum in Canada) and a target reflection of 10%. This allows the drone to fly at a high altitude and a high speed while maintaining a high point density.

Some drone LiDAR systems use low-resolution RGB cameras for the purpose of colouring the LiDAR point cloud, while others employ high-resolution RGB cameras. The latter not only provides colouring to the LiDAR point cloud, but also can be used to generate high-quality orthomosaic of the project area. In fact, combining LiDAR data with a high-resolution imaging provides greater advantages over either system alone! To ensure that there are no gaps in the coloured LiDAR point cloud, the camera field of view must be the same or larger than the LiDAR sensor field of view.

The overall system weight (including all sensors) must also be considered when selecting a drone LiDAR, as it directly affects the flight time! The higher the payload weight is, the lower the flight time! In addition, many users have already acquired the popular DJI M300/M350 and they are potentially getting a LiDAR system that can be carried by that drone. As per the DJI specifications, however, the DJI M300/M350 can carry a payload of up 2.70 kg (including all sensors). For that load, the maximum flight time for the DJI M300/M350 is estimated (by DJI) to be 31 minutes. This, however, is estimated for a new set of batteries. In addition, since it is recommended to leave about 15% of the battery charge for any emergency situation, the maximum practical flight time for a 2.7 kg payload will be around 26 minutes. As the batteries get old, that time will be further reduced. If the payload weighs more than 2.7 kg, it cannot be carried by the DJI M300/M350 and another drone must be used!

The accompanying processing software, its capabilities and ease of use must be considered when comparing different LiDAR+Imaging systems. Ideally, the software should be all-in-one, which means that it is capable of processing the captured raw data (GNSS, IMU, LiDAR, and images) without the need to invest in a third-party software or optional add-ons! The software must also be capable of producing accurate platform trajectory, point cloud and image georeferencing, filtering, and colorization. As well, the software must be capable of handling the layering problems of multiple point clouds (e.g., in-between flight paths) through an efficient strip adjustment algorithm. Moreover, the software should support rapid generation of digital ortho  and 3D models, which take advantage of images and point clouds. Furthermore, the software should support visualization of massive datasets with multiple colorization options, including elevation, intensity, RGB, and others. It must include different tools to check and analyze the obtained results. These include supporting trajectory slicing and stratification checking, which allow for detection of misalignments across the entire project. Additionally, it should be capable of elevation accuracy verification though by control points. Finally, the software should be capable of producing multiple accuracy reports to help address quality control issues.

In conclusion, when evaluating a LiDAR system, the combined performance must be considered, including data quality, productivity (coverage) over a specific period of time, and the overall system accuracy or precision. The latter must consider the combined uncertainty, i.e. the contributions of all sensors! These include positioning, attitude, range, beam footprint, incident angle, among others, as discussed above. Unfortunately, it is not uncommon to observe that the uncertainty of a LiDAR “sensor range” is mixed with the overall LiDAR “system” (payload) uncertainty. The uncertainty of the sensor “range” is about the precision of the measured distance, while the uncertainty of the overall LiDAR “system” is about the precision of the resulting point cloud coordinates! A good strategy to compare drone LiDAR systems is to collect, process and analyze actual data with the systems in question, at the same site and under the same conditions. Ideally, the site should be comprehensive, which contains heavy and light vegetated areas, asphalt, structures, and terrain elevation difference. Part of the analysis should include accuracy assessment of the coordinates at strategically-located check points. In addition, the analysis should include point density verification using non-overlapping (i.e., individual) strips from the resulting point cloud over a flat non-vegetated area (one return), a vegetated area (multiple returns and bare earth), and an area with a substantial elevation difference to verify whether the point cloud distribution satisfies the creation of an accurate DTM. Unfortunately, if this is requested as a demo, companies will likely charge fees to execute it!