Sample report

What a LandBenchmark report actually contains

This is a real report on a real parcel in Blanco County, TX (52.8 acres), rendered with the same components a user sees after analyzing land. The verdict is Review advised, from 52 measured signals, 10 of them flagged. Every value states what was observed, how, from which source, and when — most recent observation 2026-07-14. Nothing is estimated to fill a gap: what could not be measured is listed at the bottom, with the reason.

The verdict

Parcel Quality ReportPro

Verdict

Review advised — 6 things to check

Some signals were flagged — understand each one before you put money down.

  • Significant vegetation decline
  • High shrink-swell soils (foundation / slab risk)
  • Shallow bedrock/restriction (excavation, septic, foundation cost)
  • 3 contamination records near the parcel
  • Frequent extreme heat (≥ 30 days/yr at or above 35 °C — screening cutoff)
  • Parcel lies on USGS-mapped karst / soluble-rock terrain (sinkhole, cover-collapse and groundwater-vulnerability considerations)

Category scores

Higher is cleaner · 100 = nothing flagged

  • Water93
  • Climate95
  • Buildability84
  • Surroundings94
  • Access83
  • Hazard88

Each signal we measured in this category counts once. A hard flag removes its full weight; a context flag removes half. The score is the share of weight remaining. It is absolute — not benchmarked against other parcels or a regional average, because LandBenchmark has no such baseline to compare against.

Signals measured
52
Flags raised
10
Human checks
8
Imagery
2026-07-14
most recent capture

What needs attention

10 flagged signals — these drive the verdict. Flags arrive open, with their method and trust limits.

Vegetation health & trendClimate Pro · satellite0.37mean NDVI flagged

trend declining, significant (tau=-0.62, p=0.000)

Why

  • Vegetation is significantly declining
  • Investigate drought, clearing, or land degradation.

Significant vegetation decline

When

Observed 2024-12-09 · Sentinel-2 L2A · window 2019-01-01→2024-12-31 · 20m

How we measured it — method, source & limits
How

NDVI = (NIR−Red)/(NIR+Red); trend via Theil-Sen slope + Mann-Kendall significance

Evidence
Rouse et al. 1973; Sen 1968; Mann 1945/Kendall 1975
Trust

Reliable as relative trend given adequate archive

LiveSentinel-2 L2A1.7y agoHigh confidenceSource
Aspect (slope facing direction)Buildability Pro · satellite3% of slopes facing south flagged

southerly-ness index -0.46 (−1 N … +1 S); 5% of parcel is near-flat

Why

Slopes mostly face north — cooler, lower solar gain, later snow-melt.

Predominantly north-facing (reduced solar gain / colder)

How we measured it — method, source & limits
How
  • Aspect from Horn 1981 3×3 gradient: azimuth = atan2(∂z/∂y, −∂z/∂x)
  • Southerly-ness = mean cos(azimuth − 180°) over sloped pixels
Evidence
Horn 1981 (Proc. IEEE 69:14)
Trust
  • Relative aspect Reliable
  • GLO-30 is a surface (DSM) model so canopy/buildings bias aspect on vegetated/urban land
LiveUSGS 3DEP seamless DEM (bare-earth)Screening-gradeSource
Floodplain position (HAND)Water Pro · satellite98% of parcel within 5 m of drainage level flagged
  • Median HAND 1.1 m above local drainage
  • 98% of the parcel lies within 5 m of channel level

Why

  • A large share of the parcel is only a few metres above the nearest channel
  • The classic floodplain position, so check flood history and freeboard.

Much of the parcel sits near local drainage level

How we measured it — method, source & limits
How
  • HAND = terrain height above the nearest D8-routed drainage cell (Nobre et al. 2011)
  • % of parcel within 5 m of local drainage level
Evidence
Nobre et al. 2011 (J. Hydrology 404:13); Rennó et al. 2008
Trust
  • Indicative floodplain proxy
  • The channel threshold is a heuristic
  • Corroborate with FEMA / observed flood history before relying on it
LiveUSGS 3DEP seamless DEM (bare-earth)Screening-gradeSource
Utility services proximityAccess3569m to nearest grid power flagged

power ~3569 m; no water infra within radius (searched within 5327 m of the parcel)

Why

Utilities look distant — budget for grid extension or off-grid, and confirm water supply.

Grid power >2 km away (connection / extension cost)

How we measured it — method, source & limits
How

Overpass nearest power=line|substation or man_made water infrastructure within radius of centroid (haversine)

Evidence
OpenStreetMap contributors; OpenInfraMap
Trust
  • Distribution lines and buried mains are often unmapped in OSM
  • Treat as an upper bound on proximity
LiveOpenStreetMapScreening-gradeSource
Farmland & land capabilityBuildability6land capability class (1 best … 8) flagged

Tarpley (70% of map unit): Not prime farmland; capability class 6

Why

  • Classified as prime farmland
  • Productive ground, but check for ag-zoning, conservation easements or tax programs that can limit development.

Prime farmland — possible agricultural zoning / tax constraints

How we measured it — method, source & limits
How

SSURGO farmland classification + nonirrigated land-capability class (niccdcd)

Evidence
USDA-NRCS SSURGO; USDA Land Capability Classification (Klingebiel & Montgomery 1961)
Trust
  • US only
  • 'prime farmland' status can carry agricultural zoning / tax (e.g. Williamson Act) implications worth checking
LiveUSDA-NRCS SSURGOScreening-gradeSource
Expansive-soil potentialBuildability13.4% linear extensibility (LEP) flagged

Tarpley (70% of map unit): max LEP 13.4% (high shrink-swell)

Why

  • Soils shrink and swell markedly with moisture
  • A foundation-design issue (slabs, footings, drainage) to engineer for.

High shrink-swell soils (foundation / slab risk)

How we measured it — method, source & limits
How

SSURGO linear extensibility percent (LEP) of the dominant component → shrink-swell potential

Evidence
USDA-NRCS SSURGO (LEP)
Trust
  • Screening
  • LEP > 6% ≈ high shrink-swell → a foundation-design consideration, not a determination
LiveUSDA-NRCS SSURGOHigh confidenceSource
Depth to bedrock / restrictionBuildability38cm to restrictive layer flagged

Tarpley (70% of map unit): restrictive layer at ~38 cm

Why

  • A restrictive layer sits shallow
  • Expect harder excavation, tougher septic siting and possible blasting/ripping cost.

Shallow bedrock/restriction (excavation, septic, foundation cost)

How we measured it — method, source & limits
How

SSURGO depth to the shallowest restrictive layer / bedrock (corestrictions.resdept_r)

Evidence
USDA-NRCS SSURGO
Trust
  • US only
  • Shallow bedrock raises excavation, septic and foundation cost
  • Confirm with a site investigation
LiveUSDA-NRCS SSURGOHigh confidenceSource
Environmental records nearby (EPA)Surroundings3contamination records near the parcel flagged
  • Within 3 km: 9 leaking storage tank (lust), 4 hazardous waste (rcra), 35 storage tank facility, 11 permitted water discharge.
  • Of concern: JCB PLAZA (leaking storage tank (lust)) ~1225 m
  • AFB MEMORIAL HOSPITAL (leaking storage tank (lust)) ~1273 m
  • PILGRAM BUSHNELL NEWMAN WATER WELLS (leaking storage tank (lust)) ~1273 m. ⚠ Not checked this run: Toxic release (TRI).

Why

  • 3 records of known or reported contamination sit close to this parcel.
  • Off-site contamination migrates through groundwater and soil vapour, so this alone justifies a Phase-1 environmental records review before you commit.
  • This is a proximity screen over EPA's mapped records, not a Phase-1 records review.
  • It does not cover facilities that closed before these registries existed, state-agency files, or anything ever done on the parcel itself.
  • No records found here does not mean the land is clean.

3 contamination records near the parcel

How we measured it — method, source & limits
How
  • Proximity query against EPA's mapped facility registry (Brownfields, TRI toxic releases, RCRA hazardous-waste handlers, permitted water dischargers, permitted air emitters) and EPA UST Finder (reported storage-tank releases [LUST] and registered tank facilities) within 3 km of the parcel centroid, with geodesic distance to each. Records are tiered by severity: a brownfield, reported chemical release, or leaking storage tank within 1.6 km flags
  • A hazardous-waste handler or tank facility flags only within 500 m (RCRA registers every auto shop and dry cleaner)
  • Permitted air and water dischargers are reported for awareness and never flag.
Evidence
US EPA Facility Registry Service (TRI, RCRAInfo, ACRES Brownfields, NPDES, ICIS-Air); EPA UST Finder (LUST/UST)
Trust
  • A proximity screen over EPA's MAPPED records
  • Not an ASTM E1527 Phase I ESA. It does not cover historical facilities that closed before these registries existed, state-agency files, or any on-parcel history. Absence of records here is NOT evidence that a parcel is clean. Distances are to a record's registered coordinate, which is often an office or a street address rather than the release point.
LiveUS EPA Facility Registry ServiceScreening-gradeSource
Extreme heat daysHazard45days/yr Tmax ≥ 35 °C flagged

~45 days/yr ≥ 35 °C; ~1 days/yr ≥ 40 °C (ERA5 2015–2024)

Why

  • Around 45 days per year reach 35 °C and 1 reach 40 °C
  • Weigh heat stress on crops, livestock, workers and cooling load
  • The flag threshold is a screening convention, not a health standard.

Frequent extreme heat (≥ 30 days/yr at or above 35 °C — screening cutoff)

When

Open-Meteo ERA5 · window 2015-01-01→2024-12-31 · 9000m

How we measured it — method, source & limits
How

Mean days/yr with Tmax ≥ 35 °C (and ≥ 40 °C) from ERA5 daily maxima

Evidence
ERA5 (Hersbach et al. 2020, Q. J. R. Meteorol. Soc. 146:1999)
Trust
  • The ≥ 30 days/yr ≥ 35 °C flag cutoff is a screening convention, not a health or crop standard
  • 9 km grid smooths local extremes
LiveOpen-Meteo ERA51.7y agoScreening-gradeSource
Karst / soluble-rock terrainHazardCarbonate rocks at or near the land surface in a dry climateUSGS karst type flagged
  • USGS karst polygon: Carbonate rocks at or near the land surface in a dry climate
  • Glen Rose Limestone, Early Cretaceous, limestone

Why

  • This land sits on mapped soluble bedrock
  • Sinkholes, voids and rapid groundwater pathways are possible
  • Budget a geotechnical/karst survey before siting structures, wells or septic.

Parcel lies on USGS-mapped karst / soluble-rock terrain (sinkhole, cover-collapse and groundwater-vulnerability considerations)

How we measured it — method, source & limits
How

USGS 'Karst in the United States' (OFR 2014-1156) carbonate/evaporite karst polygon at the point, served from an Esri-hosted copy of the USGS digital dataset

Evidence
USGS Open-File Report 2014-1156 (Weary & Doctor)
Trust
  • Small-scale national compilation
  • A regional soluble-rock screen, not a site sinkhole survey
  • Volcanic/piping pseudokarst layers are not screened here
  • Layer is hosted by Esri (not usgs.gov), schema-verified against the USGS publication
LiveUSGS karst compilationHigh confidenceSource

Water

Flood / surface-water historyWater Pro · satellite0% wet-frequency (AOI mean)

peak 0% of parcel wet on 2024-12-09; 24 clear scenes 2019–2024

Why

No recurring surface water detected over the period — low observed flood signal.

When

Observed 2024-12-09 · Sentinel-2 L2A · window 2019-01-01→2024-12-31 · 20m

How we measured it — method, source & limits
How
  • MNDWI = (Green−SWIR)/(Green+SWIR), water where MNDWI>0
  • Water-occurrence over clear observations (JRC construct)
Evidence
Xu 2006; Pekel et al. 2016 (JRC Global Surface Water)
Trust

Reliable (open water); corroborated by the Sentinel-1 SAR signal (cloud-robust)

LiveSentinel-2 L2A1.7y agoHigh confidenceSource
Ponding / wetness index (TWI)Water Pro · satellite0% of parcel prone to water pooling

median TWI 6.5, max 11.0; 0% of the parcel exceeds TWI 15 (saturation-prone)

Why

Topography sheds water fairly evenly — no strong ponding tendency observed.

How we measured it — method, source & limits
How
  • TWI = ln(a / tanβ), a = specific catchment area from D8 flow accumulation, β = local slope
  • % of parcel above the saturation-prone threshold (TWI > 15)
Evidence
Beven & Kirkby 1979 (Hydrol. Sci. Bull. 24:43)
Trust
  • Relative wetness index
  • Sensitive to DEM resolution
  • A coarse DEM smooths micro-topography, so treat as a screening cue, not a drainage design
LiveUSGS 3DEP seamless DEM (bare-earth)Screening-gradeSource
Wetlands (NWI)WaterNone mappedNWI wetland type

No NWI wetland polygon intersects the parcel

Why

  • No mapped wetland at the point
  • But NWI can miss small or forested wetlands, so a field check still governs any Clean Water Act permitting.
How we measured it — method, source & limits
How

USFWS National Wetlands Inventory wetland polygon at the point (ArcGIS REST)

Evidence
USFWS National Wetlands Inventory (NWI)
Trust
  • US inventory flag only
  • A jurisdictional wetland delineation requires a professional
  • NWI can miss small/forested wetlands
LiveUSFWS NWIHigh confidenceSource
Water stress (WRI Aqueduct)WaterMedium - High (20-40%)baseline water-stress category

baseline water stress: Medium - High (20-40%) for Pfafstetter basin 751810, United States (withdrawals vs available supply)

Why

  • Baseline water stress here is Medium - High (20-40%)
  • Limited regional competition for water, but this is a basin-level indicator, not a legal water right
  • Confirm local availability and permits.
How we measured it — method, source & limits
How

Baseline water stress (ratio of withdrawals to available supply) of the WRI Aqueduct 4.0 sub-basin containing the parcel

Evidence
WRI Aqueduct 4.0 (Kuzma et al. 2023)
Trust
  • Basin-level indicator of regional water competition
  • NOT a legal water-right
  • Confirm actual rights/permits in local records
LiveWRI Aqueduct 4.0High confidenceSource
Surface-water seasonality (JRC)Water0% of parcel with water ≥1 month/yr
  • Max 0 months/yr of standing water
  • Permanent (12-month) water on 0% of parcel (JRC seasonality layer 2020)

Why

  • Little to no seasonal open water mapped on the parcel
  • Corroborates a low standing-water signal.

When

JRC Global Surface Water v1.3 (Landsat) · window 2020-01-01→2020-12-31 · 30m

How we measured it — method, source & limits
How
  • JRC Global Surface Water `seasonality` layer: per-pixel count of months (1-12) with open water in the layer year
  • Parcel stat = % of pixels with water ≥1 month/yr (max months and permanent 12-month share reported in detail)
Evidence
Pekel, Cottam, Gorelick & Belward 2016 (Nature 540:418) — JRC Global Surface Water v1.3
Trust
  • 30 m Landsat-derived (archive 1984-2020
  • Seasonality layer = calendar 2020). Detects OPEN water only
  • Misses water under canopy and channels narrower than ~30 m
LiveJRC Global Surface Water v1.3 (Landsat)5.7y agoHigh confidenceSource
Current drought status (USDM)WaterD0 Abnormally DryUSDM category (None, D0 Abnormally Dry … D4 Exceptional)

Blanco County, TX: D0 Abnormally Dry across 55% of the county (USDM map of 2026-07-14)

Why

  • Current US Drought Monitor status here is D0 Abnormally Dry
  • A weekly snapshot of present conditions
  • Long-term water availability needs its own review.

When

Observed 2026-07-14 · US Drought Monitor

How we measured it — method, source & limits
How
  • Current US Drought Monitor category for the parcel's county (dominant D0–D4 class by exclusive area share
  • County FIPS via the FCC census-block API)
Evidence
US Drought Monitor (NDMC/USDA/NOAA)
Trust
  • Weekly national product at county scale
  • Current conditions, not a long-term water-supply determination
LiveUS Drought Monitor2mo agoHigh confidenceSource

Buildability

Slope & buildable areaBuildability Pro · satellite3.1% median slope

buildable (<8%) 99% of parcel; p90 slope 5%

Why

Gentle gradients across most of the parcel — favourable for building.

How we measured it — method, source & limits
How
  • Slope from Copernicus GLO-30 DEM (Horn 1981 gradient)
  • Buildable = % of parcel under 8% slope
Evidence
Horn 1981; USDA NRCS slope classes
Trust
  • Slope Reliable
  • 'buildable' cut-off Indicative (planning convention). GLO-30 smooths <30-90m → use 3DEP LiDAR for US grading-scale
LiveUSGS 3DEP seamless DEM (bare-earth)High confidenceSource
Elevation & local reliefBuildability Pro · satellite14m relief (max−min)

elevation 379–393 m, median 385 m (USGS 3DEP seamless DEM (bare-earth))

Why

Modest local relief — straightforward siting.

How we measured it — method, source & limits
How

Local relief = max−min elevation, plus median absolute elevation, over the parcel from the GLO-30 DEM

Evidence
Copernicus GLO-30 DEM (TanDEM-X 2011–2015)
Trust

~4 m vertical accuracy; surface (DSM) not bare-earth — prefer 3DEP LiDAR in the US

LiveUSGS 3DEP seamless DEM (bare-earth)High confidenceSource
LandBenchmark ruggedness (TRI)Buildability Pro · satellite0.9m TRI (mean)

TRI mean 1 m over the parcel (Riley classes: <80 level … >959 extremely rugged)

Why

Smooth terrain — low ruggedness, easy to work.

How we measured it — method, source & limits
How

LandBenchmark Ruggedness Index (Riley et al. 1999): TRI = sqrt(Σ(z_neighbour − z_centre)²) over the 8-cell neighbourhood, mean over parcel

Evidence
Riley et al. 1999 (Intermountain J. Sci. 5:23); Sappington et al. 2007 (JWM 71:1419)
Trust

Screening index; correlates with slope. VRM (Sappington 2007) decorrelates if needed

LiveUSGS 3DEP seamless DEM (bare-earth)High confidenceSource
Usable acreageBuildability Pro · satellite54.54acres usable (<12% slope)
  • Of 54.7 ac total
  • 48.88 ac (<5% slope), 53.96 ac (<8% slope), 54.54 ac (<12% slope), 54.7 ac (<15% slope)
  • No flood or wetland area on the parcel

Why

54.54 of 54.7 acres (99.7%) remain usable at the 12% slope convention after flood and wetland exclusions.

How we measured it — method, source & limits
How
  • Slope from the DEM (Horn 1981). The parcel polygon is rasterised onto the DEM grid
  • Cells are counted usable when slope is under the threshold AND they fall outside the FEMA Special Flood Hazard Area (NFHL layer 28, SFHA_TF='T') and outside mapped USFWS National Wetlands Inventory polygons. Usable acres = usable cells × cell ground area. Slope cutoffs are planning conventions (5/8/12/15%), reported as a curve rather than a single figure.
Evidence
Horn, B.K.P. (1981) Hill shading and the reflectance map. FEMA National Flood Hazard Layer. U.S. Fish & Wildlife Service National Wetlands Inventory.
Trust

Screening estimate, not a site plan. The DEM is a gridded surface model (indicative, not survey-grade), NWI mapping is not a jurisdictional wetland determination, and FEMA zones are regulatory maps rather than observed flooding. Setbacks, easements, and local grading rules are not subtracted. Confirm with a licensed surveyor before relying on acreage.

LiveUSGS 3DEP seamless DEM (bare-earth)Screening-gradeSource
Erosion potential (RUSLE LS)Buildability Pro · satellite0.3LS factor (median terrain erosivity)

median LS 0.3; 0% of parcel LS>10 (steep/long slopes)

Why

Gentle, short slopes — low terrain-driven erosion potential.

How we measured it — method, source & limits
How
  • RUSLE topographic factor LS = (aₛ/22.13)^0.4·(sinβ/0.0896)^1.3 (Moore & Burch 1986), aₛ = specific catchment area from D8 flow accumulation, β = slope
  • Relative terrain-driven erosion potential
Evidence
Moore & Burch 1986 (SSSAJ 50:1294); Wischmeier & Smith 1978 (RUSLE, USDA AH-537)
Trust
  • Topographic (LS) factor ONLY
  • Rainfall (R), soil (K), cover (C) and practice (P) are not included, so this is RELATIVE terrain erosivity, not an absolute soil-loss rate
  • DEM-resolution sensitive
LiveUSGS 3DEP seamless DEM (bare-earth)Screening-gradeSource
Landform position (valley / ridge)Buildability Pro · satellitemid-slope / flatdominant landform (TPI)

11% valley, 12% ridge, 78% mid/flat (TPI ±1σ, 7-cell window)

Why

  • Dominant landform: mid-slope / flat.
  • Ridges are wind-exposed
  • Valleys pool cold air and water
  • Site the build accordingly.
How we measured it — method, source & limits
How
  • Topographic Position Index = elevation minus the local neighbourhood mean (Weiss 2001)
  • Classed valley / mid-slope / ridge by ±1 standard deviation of TPI over the parcel
Evidence
Weiss 2001 (ESRI User Conf.); Guisan et al. 1999
Trust
  • Relative landform position at the sampled window scale
  • Valley bottoms pool cold air/frost and water, ridges are wind-exposed
  • A microclimate/siting cue, not a hazard determination
LiveUSGS 3DEP seamless DEM (bare-earth)Screening-gradeSource
Soil drainage classBuildabilityWell drainednatural drainage class

Tarpley (70% of map unit): Well drained

Why

Dominant soil is well drained — generally workable drainage (confirm on site).

How we measured it — method, source & limits
How

USDA-NRCS SSURGO natural drainage class of the dominant map-unit component (Soil Data Access)

Evidence
USDA-NRCS SSURGO
Trust

US only; map-unit generalisation (not a site boring) — on-site soils vary

LiveUSDA-NRCS SSURGOHigh confidenceSource
Septic suitability (perc screen)Buildability1.3µm/s Ksat (indicative perc)

Tarpley (70% of map unit): mean Ksat 1.3 µm/s → moderate percolation

Why

  • Permeability is in a workable range for a conventional septic system
  • A certified perc test still governs.
How we measured it — method, source & limits
How

Indicative percolation from SSURGO saturated hydraulic conductivity (Ksat) of the dominant component

Evidence
USDA-NRCS SSURGO (Ksat)
Trust
  • Screening only
  • A certified percolation/perc test is required for any septic permit
  • Ksat is a lab-derived proxy
LiveUSDA-NRCS SSURGOScreening-gradeSource
Soil productivity (NCCPI)Buildability20/100 (NCCPI v3.0)

very low inherent productivity — poorly suited to commodity crops

Why

  • USDA rates this map unit 20/100 for inherent commodity-crop productivity (very low).
  • This describes the soil's natural capability, not what the land is worth or what you may build on it.
How we measured it — method, source & limits
How

USDA-NRCS National Commodity Crop Productivity Index (NCCPI v3.0), 0–1. Component values (cointerp.interphr at ruledepth 0) are aggregated to the map unit weighted by each component's share of it (component.comppct_r), for the map unit under the parcel centroid.

Evidence
Dobos, R.R., Sinclair, H.R., Robotham, M.P. (2012) National Commodity Crop Productivity Index (NCCPI) User Guide. USDA-NRCS.
Trust
  • US only (SSURGO coverage). A map-unit generalisation sampled at the parcel centroid, not a soil test of your building site or field. NCCPI rates inherent commodity-crop capability
  • It does not account for irrigation, drainage improvements, or management history.
LiveUSDA-NRCS SSURGO (NCCPI v3.0)High confidenceSource
Soil texture (USDA)Buildability Pro · satelliteClay LoamUSDA texture class

Clay Loam: clay 29%, sand 30%, silt 41% (0–30 cm)

Why

  • Topsoil is clay loam (~29% clay / 30% sand / 41% silt).
  • A workable, moderate texture for building and growing (a 250 m model estimate
  • Confirm on site).
How we measured it — method, source & limits
How

USDA soil texture class from SoilGrids 2.0 clay/sand/silt fractions, 0–30 cm depth-weighted mean

Evidence
SoilGrids 2.0 (Poggio et al. 2021 SOIL 7:217)
Trust
  • Global 250 m model prediction (not a field survey)
  • Heavy clay → shrink-swell & drainage issues, pure sand → low water/nutrient retention. In the US, SSURGO (see soil signals) is more authoritative
LiveISRIC SoilGrids 2.0Screening-gradeSource
Soil pH (H2O)Buildability Pro · satellite7.2pH (H2O)

0–30 cm mean pH ~7.2 (near-neutral)

Why

  • Topsoil pH is about 7.2
  • Near-neutral. A workable range for most crops and construction (a 250 m model estimate
  • A lab test governs).
How we measured it — method, source & limits
How

Soil pH in water from SoilGrids 2.0, 0–30 cm depth-weighted mean

Evidence
SoilGrids 2.0 (Poggio et al. 2021 SOIL 7:217)
Trust
  • Global 250 m model
  • Strongly acidic (<5) or alkaline (>8.5) soils limit crops and can affect concrete/rebar
  • Confirm with a lab test
LiveISRIC SoilGrids 2.0Screening-gradeSource
Soil organic carbonBuildability Pro · satellite15.6g/kg SOC

0–30 cm mean SOC ~15.6 g/kg (~1.56% organic carbon) — moderate for topsoil

Why

  • Topsoil holds about 15.6 g/kg organic carbon (~1.56%), a moderate organic-matter level
  • A fertility/soil-health proxy from a 250 m model, not a nutrient test.
How we measured it — method, source & limits
How

Soil organic carbon content from SoilGrids 2.0, 0–30 cm depth-weighted mean

Evidence
SoilGrids 2.0 (Poggio et al. 2021 SOIL 7:217)
Trust

Global 250 m model; a fertility/organic-matter proxy, not a nutrient test

LiveISRIC SoilGrids 2.0Screening-gradeSource

Access

Road access & distanceAccess54m to nearest road

nearest road (service) ~54 m from parcel boundary

Why

A mapped road runs close to the parcel — access is plausible (confirm legal frontage).

How we measured it — method, source & limits
How

Overpass nearest highway=* distance from the parcel centroid (haversine)

Evidence
OpenStreetMap contributors; Overpass API
Trust

highway class = importance, NOT surface quality; legal/deeded access needs a title search

LiveOpenStreetMapScreening-gradeSource
Gas transmission pipeline proximityAccess

No EIA-mapped gas transmission pipeline within ~3 km

Why

  • No mapped transmission-level gas pipeline nearby
  • No pipeline easement/safety screen triggered
  • Note this says nothing about local gas distribution service to the parcel.
How we measured it — method, source & limits
How

Distance to nearest EIA-mapped natural-gas interstate/intrastate transmission pipeline within ~3 km (ArcGIS FeatureServer distance query + local point-to-segment distance)

Evidence
US EIA Natural Gas Interstate & Intrastate Pipelines (via HIFLD Open)
Trust
  • Transmission-level network only
  • A nearby line does NOT mean connectable gas service (that is the local distribution utility)
  • Close proximity is a safety/easement consideration, and our <300 m flag is a screening cut in the spirit of PHMSA consultation zones, not a regulatory determination
LiveEIA gas pipelines (HIFLD)Screening-gradeSource

Hazard

Seismic design demandHazard0.05g (S_DS design acceleration)

S_DS 0.05 g; Seismic Design Category A

Why

Moderate-to-low seismic design demand for standard construction.

How we measured it — method, source & limits
How

USGS ASCE 7-16 seismic design values (S_DS design spectral acceleration and Seismic Design Category) at the point, Risk Category II / Site Class D

Evidence
USGS Seismic Design Web Services; ASCE 7-16
Trust
  • US & territories
  • Design-level ground motion for code compliance
  • Not a site-specific fault or liquefaction study
LiveUSGS ASCE 7-16High confidenceSource
Wildfire hazard potential (USFS)HazardLowWHP class (Very Low…Very High)

USFS WHP 2023 class: Low (class 2 of 5)

Why

  • Wildfire hazard potential is Low
  • A lower-hazard band regionally, though local fuels, slope and weather still matter.
How we measured it — method, source & limits
How

USFS Wildfire Hazard Potential 5-class at the point (FSim + LANDFIRE fuels)

Evidence
USFS Wildfire Hazard Potential 2023 (270 m)
Trust

US only at 270 m — regional context, not a site-level fire assessment

LiveUSFS WHPHigh confidenceSource
Radon zone (EPA)HazardZone 3EPA radon zone (1 highest–3 lowest)

Blanco County, Texas: EPA radon Zone 3 — lowest predicted potential (<2 pCi/L)

Why

  • This county is EPA radon Zone 3 (lower predicted potential)
  • Levels still vary house to house, so an in-home test is the only confirmation.
How we measured it — method, source & limits
How

EPA Map of Radon Zones — predicted county radon potential (Zone 1 ≥4 pCi/L … Zone 3 <2)

Evidence
EPA Map of Radon Zones (EPA-402-R-93-071)
Trust
  • County-level screen only
  • Indoor radon varies house to house
  • Only an in-home test confirms actual levels
LiveEPA Map of Radon ZonesHigh confidenceSource
Earthquake history (observed)Hazard0M≥4.5 events within 100 km since 1975

no M≥4.5 earthquakes within 100 km of the centroid since 1975 (USGS ComCat)

Why

  • A quiet observed record
  • No M≥4.5 earthquakes within 100 km since 1975.
  • Catalog completeness varies by region, and a quiet catalog is not zero hazard
  • The national building code still sets the design values.

When

USGS ComCat (FDSN event service) · window 1975-01-01→2026-07-23

How we measured it — method, source & limits
How

USGS FDSN event service: count + largest + most recent M≥4.5 event within 100 km of the parcel centroid since 1975 (count endpoint + magnitude-ordered query)

Evidence
USGS Comprehensive Catalog (ComCat), FDSN event service
Trust
  • Observed catalog
  • Completeness varies by region/era
  • Hazard DESIGN values need the national code (US: ASCE 7 signal)
LiveUSGS ComCat (FDSN event service)1mo agoScreening-gradeSource
Volcanic proximityHazard807.6km to nearest Holocene volcano

nearest Holocene volcano: Carrizozo, United States at 808 km (last known eruption 3250 BCE)

Why

  • The nearest Holocene volcano (Carrizozo, United States) is 808 km away
  • Outside the typical near-field hazard range, though heavy regional ashfall from a large eruption can travel farther
  • A proximity screen, not a hazard-zone map.
How we measured it — method, source & limits
How

Haversine distance from the parcel centroid to the nearest Holocene volcano in the Smithsonian GVP WFS (bbox ±3°, widened to ±8° if empty)

Evidence
Smithsonian Global Volcanism Program, Volcanoes of the World
Trust
  • Proximity screen to Holocene volcanic centers
  • Actual hazard footprints (ashfall/lahar) need national volcanic-hazard maps
LiveSmithsonian GVP Volcanoes of the World (Holocene)Screening-gradeSource
Wildfire burn history (MODIS)Hazard Pro · satellite0distinct burn months in last ~6 yr
  • No burned area detected in 57 monthly composites 2020-2026 (500 m
  • Small burns can be missed)

Why

  • No satellite-detected burn in ~6 years of monthly burned-area maps
  • Low observed fire history (small burns below 500 m scale can escape detection).

When

MODIS Terra+Aqua (MCD64A1 v6.1) · window 2020-07-23→2026-07-23 · 500m

How we measured it — method, source & limits
How
  • MODIS MCD64A1 monthly burned-area: burned pixel = Burn_Date > 0 (day-of-year of burn
  • 0 = unburned, negatives = water/unmapped fill)
  • Parcel stat = distinct burn months over the last ~6 years, plus % of parcel pixels ever burned
Evidence
Giglio et al. 2018 (Remote Sens. Environ. 217:72) — MCD64A1 Collection 6.1
Trust
  • 500 m resolution
  • Reliably maps large burns but misses small, patchy or low-intensity fires
  • Read as regional burn history, not a parcel-level burn determination
LiveMODIS Terra+Aqua (MCD64A1 v6.1)1mo agoHigh confidenceSource

Climate

Climate normals (~10 yr)Climate20.1°C mean annual temp

mean annual temp 20.1 °C; annual precipitation ~900 mm (2015–2024, ERA5)

Why

  • Regional climate averages ~20 °C and ~900 mm rain/yr
  • Informs crop, heating/cooling and water planning.

When

Open-Meteo ERA5 · window 2015-01-01→2024-12-31 · 9000m

How we measured it — method, source & limits
How

~10 yr of daily 2 m mean temperature and precipitation from ERA5 reanalysis (Open-Meteo Archive) at centroid → mean annual temperature + annual precipitation

Evidence
Hersbach et al. 2020 (ERA5)
Trust

~9 km reanalysis grid — regional context, not microclimate; WorldClim/station data refine

LiveOpen-Meteo ERA51.7y agoHigh confidenceSource
Solar PV yieldClimate1579kWh/kWp·yr

optimal tilt 29°; 1 kWp crystalline-Si, 14% system loss (PVGIS SARAH)

Why

About 1579 kWh per kWp per year — a solid solar resource for on-site PV.

How we measured it — method, source & limits
How

PVGIS PV performance model (optimally-inclined 1 kWp crystalline-Si) → annual specific yield kWh/kWp·yr at centroid

Evidence
Huld et al. 2012 (PVGIS SARAH), Solar Energy 86:1803
Trust

Modelled from satellite irradiance; on-site shading/soiling need a site survey

LivePVGISHigh confidenceSource
Wind resource (100 m)Climate6.2m/s mean @100 m

mean 100 m wind ~6.2 m/s (moderate); ERA5 2021–2023

Why

  • About 6.2 m/s average wind at 100 m
  • A moderate resource
  • Informs small-wind potential and exposure/shelter planning.

When

Open-Meteo ERA5 · window 2021-01-01→2023-12-31 · 9000m

How we measured it — method, source & limits
How

Mean 100 m wind speed from ERA5 reanalysis (Open-Meteo Archive), multi-year hourly average

Evidence
Hersbach et al. 2020 (ERA5, Q. J. R. Meteorol. Soc. 146:1999)
Trust
  • ~9 km reanalysis → regional resource, not hub-height yield
  • A met mast or the Global Wind Atlas microscale model refines it before any turbine decision
LiveOpen-Meteo ERA52.7y agoScreening-gradeSource
Growing season (frost-free days)Climate355frost-free days/yr (Tmin > 0 °C)
  • ~355 frost-free days/yr
  • Mean last spring frost ~Feb 18, first autumn frost ~Dec 1 (ERA5 2015–2024)

Why

  • About 355 frost-free days per year
  • Sets which crops and how many cycles are viable
  • On-site frost pockets can be shorter, so confirm the local last/first-frost dates.

When

Open-Meteo ERA5 · window 2015-01-01→2024-12-31 · 9000m

How we measured it — method, source & limits
How

Mean count of days/yr with Tmin > 0 °C (frost-free season) plus mean last-spring / first-autumn frost day-of-year, from ERA5 daily minima

Evidence
ERA5 (Hersbach et al. 2020, Q. J. R. Meteorol. Soc. 146:1999); ETCCDI growing-season indices
Trust
  • 9 km reanalysis
  • Local frost pockets vary
  • On-site microclimate (cold-air drainage, slope, aspect) governs actual planting dates
LiveOpen-Meteo ERA51.7y agoHigh confidenceSource
Snow daysClimate2days/yr with snowfall

~2 snowfall days/yr; ~2 cm annual snowfall (ERA5 2015–2024)

Why

  • About 2 snow days and ~2 cm of snow per year
  • Informs access, heating and roof/structure design.
  • This is climatology only
  • Structural snow LOAD must come from the local code (e.g. ASCE 7 ground snow load).

When

Open-Meteo ERA5 · window 2015-01-01→2024-12-31 · 9000m

How we measured it — method, source & limits
How

Mean days/yr with snowfall > 0 and mean annual snowfall depth (cm) from ERA5 daily snowfall_sum

Evidence
ERA5 (Hersbach et al. 2020, Q. J. R. Meteorol. Soc. 146:1999)
Trust
  • Snow CLIMATOLOGY only
  • Structural snow LOAD for design needs the local code value (e.g. ASCE 7 ground snow load), not this frequency
LiveOpen-Meteo ERA51.7y agoHigh confidenceSource
Aridity index (UNEP)Climate0.6AI = P / ET0
  • AI 0.60
  • UNEP 'dry sub-humid' (P ~900 mm/yr, ET0 ~1503 mm/yr
  • Bands: hyper-arid <0.05, arid 0.05–0.20, semi-arid 0.20–0.50, dry sub-humid 0.50–0.65, humid >0.65)

Why

  • Aridity Index 0.60 places this in the UNEP 'dry sub-humid' class
  • Rainfall broadly meets or exceeds evaporative demand for much of the year (still check seasonal timing).

When

Open-Meteo ERA5 · window 2015-01-01→2024-12-31 · 9000m

How we measured it — method, source & limits
How

UNEP Aridity Index AI = mean annual precipitation / mean annual reference evapotranspiration (FAO-56 Penman–Monteith ET0), from ERA5 daily

Evidence
UNEP 1992 (World Atlas of Desertification); FAO-56 Penman–Monteith ET0; ERA5 (Hersbach et al. 2020)
Trust
  • AI < 0.20 is the UNEP 'Arid' class (a recognised standard)
  • A 9 km climatology
  • A well permit/water balance still needs local data
LiveOpen-Meteo ERA51.7y agoHigh confidenceSource
Rainfall seasonality (BIO15)Climate40CV % of monthly precip
  • Monthly-precip CV 40% (WorldClim BIO15)
  • Wettest May ~158 mm, driest Jul ~41 mm (ERA5 2015–2024)

Why

  • Rainfall seasonality CV of 40%
  • Moderately spread across the year.
  • Wettest May, driest Jul.

When

Open-Meteo ERA5 · window 2015-01-01→2024-12-31 · 9000m

How we measured it — method, source & limits
How

Coefficient of variation of the 12 monthly precipitation normals (WorldClim BIO15 construct) over the ~10 yr window

Evidence
Fick & Hijmans 2017 (WorldClim 2, Int. J. Climatol. 37:4302); O'Donnell & Ignizio 2012 (BIO15)
Trust
  • Higher CV = more concentrated (seasonal) rainfall
  • A 9 km grid smooths orographic gradients
  • Treat as regional context
LiveOpen-Meteo ERA51.7y agoHigh confidenceSource
Köppen–Geiger climate classClimateCfaKöppen–Geiger class
  • Köppen–Geiger Cfa (humid subtropical)
  • From monthly T & P normals (Beck et al.
  • 2018 rules, ERA5 2015–2024)

Why

  • Climate class Cfa (humid subtropical)
  • A compact summary of the temperature/rainfall regime useful for matching crops, vegetation and building practice
  • Computed from a 9 km grid, so borderline sites can shift a letter.

When

Open-Meteo ERA5 · window 2015-01-01→2024-12-31 · 9000m

How we measured it — method, source & limits
How

Köppen–Geiger climate class computed from the 12 monthly temperature ((Tmin+Tmax)/2) and precipitation normals using the Beck et al. 2018 rules

Evidence
Beck et al. 2018 (Sci. Data 5:180214); Köppen–Geiger
Trust
  • Computed from 9 km ERA5 normals with T approximated as (Tmin+Tmax)/2
  • Class boundaries are approximate at local scale
  • A full three-letter class is emitted but borderline sites can shift a letter
LiveOpen-Meteo ERA51.7y agoHigh confidenceSource
Land cover (ESA WorldCover)Climate53% of parcel is Tree cover (dominant class)
  • Top-3: Tree cover 53%, Grassland 36%, Built-up 10%
  • Tree cover 53% of parcel (WorldCover 2021 v200)

Why

  • Predominantly tree cover (53%), tree cover 53%
  • Informs clearing effort, shading and land use context.

When

ESA WorldCover 10 m (2021, v200, Sentinel-1+2) · window 2021-01-01→2021-12-31 · 10m

How we measured it — method, source & limits
How
  • ESA WorldCover 10 m `map` asset: dominant class % + top-3 class breakdown over the parcel from the verified class table (10 Tree cover … 100 Moss and lichen
  • 0 = nodata)
  • Tree-cover % reported in detail
Evidence
Zanaga et al. 2022 (ESA WorldCover 10 m v200)
Trust
  • 10 m single-epoch class map (latest hosted year, 2021 v200)
  • Mixed pixels and parcel edges misclassify
  • Verify the dominant class against recent imagery
LiveESA WorldCover 10 m (2021, v200, Sentinel-1+2)4.7y agoHigh confidenceSource

Surroundings

Neighbouring land useSurroundings

no industrial/landfill/quarry/works within 500 m of the parcel (0 land uses seen nearby)

Why

No mapped industrial/waste/extraction land use in the immediate surroundings.

How we measured it — method, source & limits
How
  • Overpass proximity query: nearest landuse=industrial|landfill|quarry|farmland or man_made=works within ~500 m of centroid
  • Nearest-nuisance distance (haversine)
Evidence
OpenStreetMap contributors; Overpass API
Trust
  • OSM completeness varies by region
  • Absence ≠ confirmed clear. EPA FRS adds US industrial sites
LiveOpenStreetMapScreening-gradeSource
Air quality (PM2.5)Surroundings8.7µg/m³ mean PM2.5 (recent ~90 d)
  • Recent 90-day mean PM2.5 ~9 µg/m³ (annual health guidelines: WHO 5, US EPA 9 µg/m³
  • This is a seasonal snapshot, not an annual normal)

Why

Fine-particulate levels are in a typical range for the recent period (a seasonal snapshot, not an annual normal).

How we measured it — method, source & limits
How

Recent-period mean surface PM2.5 from CAMS (Copernicus Atmosphere Monitoring Service) via the Open-Meteo Air-Quality API

Evidence
CAMS — Copernicus Atmosphere Monitoring Service (ECMWF)
Trust
  • A recent ~90-day mean (not a full annual normal) on a model grid, not a site monitor
  • Treat as regional context
LiveCAMS (Open-Meteo)ContextSource
Protected / conservation areasSurroundings541m to nearest protected area
  • Nearest: Lyndon B. Johnson National Historical Park (Historic or Cultural Area) ~541 m
  • 2 PAD-US designation(s) within 3000 m

Why

  • A protected area is mapped ~541 m away
  • Unlikely to restrict the parcel directly, but check buffer rules.
How we measured it — method, source & limits
How
  • USGS PAD-US v4 protected-area polygons at the point and within 3 km (GAP status 1-3
  • Fee, Designation and Easement categories), ArcGIS REST
Evidence
USGS Protected Areas Database of the United States (PAD-US) v4
Trust
  • US only. GAP status 1-3 is USGS's own definition of land carrying a mandate for protection
  • GAP 4 (most municipal parks) is excluded because it carries none. Proclamation boundaries are excluded
  • They enclose private land. Distance is measured to a boundary generalized to ~5 m, so treat sub-10 m distances as adjacency, not survey.
LiveUSGS PAD-US v4Screening-gradeSource
Superfund proximity (EPA NPL)Surroundings

No EPA Superfund NPL site within ~8 km

Why

  • No federal Superfund (NPL) site mapped nearby
  • But on-parcel history still needs a Phase I ESA
  • The NPL lists only the worst federal sites.
How we measured it — method, source & limits
How

Distance to nearest EPA Superfund National Priorities List (NPL) site within ~8 km (EPA ArcGIS)

Evidence
US EPA Superfund NPL / Facility Registry Service
Trust
  • US EPA coverage only
  • Nearby ≠ on-parcel contamination and on-parcel history needs a Phase I ESA
LiveUS EPA Superfund/FRSScreening-gradeSource
Agricultural legacy (orchard/vineyard residue)Surroundingsnone observedorchard/vineyard years in the CDL record
  • USDA CDL land cover across the parcel, 2008–2023
  • 2008: Deciduous Forest, 2015: Shrubland, 2023: Shrubland.

Why

  • No tree or vine crop appears in the USDA cropland record for this parcel.
  • Note that the record begins in 2008, and the orchard-era pesticides that leave lead and arsenic in soil were applied before 1950
  • So this is not evidence that the parcel was never an orchard.
  • Historical aerial photography and a records review are what answer that.

When

USDA NASS Cropland Data Layer · window 2008-01-01→2023-12-31 · 30m

How we measured it — method, source & limits
How

USDA NASS Cropland Data Layer sampled at five points across the parcel (centre + quarter points) in 2008, 2015 and 2023. A tree or vine crop in any sample raises a legacy-residue flag, because orchards and vineyards were historically treated with lead-arsenate insecticide, whose lead and arsenic do not degrade and persist in surface soil.

Evidence
USDA NASS Cropland Data Layer; Peryea, F.J. (1998) Historical use of lead arsenate insecticides, resulting soil contamination and implications for soil remediation, 16th World Congress of Soil Science
Trust
  • A screening indicator, never a finding of contamination
  • Only a laboratory soil test can establish that. Five 30 m samples per year, so a small orchard corner can still be missed. The CDL record begins in 2008, while the lead-arsenate era ended around 1950: the period that created the risk is invisible to this dataset. Absence of an orchard here is NOT evidence of no orchard history
  • Historical aerial photography and a records review are what settle that. The USDA CropScape service is intermittently unavailable
  • When it does not answer, this signal is absent from the report and listed as unavailable rather than reported as 'no orchard'.
LiveUSDA NASS Cropland Data Layer2.7y agoScreening-gradeSource
Regulatory-review triggersSurroundings0regulatory triggers

No designated critical habitat, National Register listing, or air-quality nonattainment area at this parcel.

Why

  • None of the three federal designations we screen appear here.
  • This is not a clearance: state and local overlays, the coastal zone (which has no free national dataset), tribal consultation, and project-specific permits are outside this screen.
  • LandBenchmark flags triggers
  • It does not certify compliance.
  • Whether your project actually requires review depends on the project, the federal nexus, and the permitting agency
  • Ask a land-use attorney before you rely on this.
How we measured it — method, source & limits
How
  • Point-in-polygon and proximity queries against three federal designations: USFWS designated critical habitat (final), National Park Service National Register of Historic Places listings within 500 m, and EPA air-quality nonattainment areas. Each is reported as a possible trigger for environmental review
  • Not as a compliance determination.
Evidence
USFWS Critical Habitat (ESA §4); National Park Service National Register of Historic Places; US EPA Green Book nonattainment areas (Clean Air Act)
Trust
  • LandBenchmark FLAGS triggers
  • It does not certify compliance. Whether a project requires ESA Section 7 consultation, NHPA Section 106 review, or nonattainment New Source Review depends on the project, the federal nexus, and the permitting agency
  • Ask a land-use attorney. Designated critical habitat does not by itself prohibit private activity without a federal nexus. The coastal zone is NOT screened: it is defined state by state and no free national service publishes it.
LiveUSFWS / NPS / EPA designationsScreening-gradeSource
Historical land-use timelineSurroundings Pro · satellite0changes detected, 1985–2026
  • No abrupt change in vegetation or surface water across 9 epochs, 1985–2026.
  • The parcel's surface has been stable at 30 m resolution.

Why

  • Nothing in the satellite archive suggests a prior disturbance on this parcel.
  • That is not a clean bill of health: 30 m pixels miss small features, and buried contamination has no surface signature at all.
  • A Phase-1 environmental records review covers what imagery cannot see.

When

Landsat 5/7/8/9 Collection-2 Level-2 · window 1985-01-01→2026-07-23 · 30m

How we measured it — method, source & limits
How

Landsat Collection-2 Level-2 surface reflectance, 1985–present, sampled in 5-year epochs. Each epoch uses the 3 least-cloudy scenes inside the same peak-canopy window, so epochs are seasonally comparable. Cloud, cloud-shadow, cirrus, snow and fill pixels are masked per-pixel from the Landsat QA band. Per epoch we take the per-pixel maximum NDVI = (NIR−Red)/(NIR+Red) (peak canopy) and the fraction of the parcel whose median MNDWI = (Green−SWIR)/(Green+SWIR) exceeds 0 while peak NDVI stays below 0.2 (standing water is wet AND unvegetated). A step of ≥0.25 NDVI or ≥0.15 water fraction between consecutive epochs is reported as an observed change. The cause is NOT inferred.

Evidence
Rouse et al. 1973 (NDVI); Xu 2006 (MNDWI); USGS Landsat Collection 2 Level-2 Surface Reflectance
Trust
  • Observed change, not an explanation. Clearing, excavation, fire, demolition, drought, harvest and ploughing can all produce the same reflectance step
  • Imagery cannot distinguish them. 30 m pixels miss small features. Persistent cloud can leave an epoch with no usable observation, which is reported as a gap rather than as stability. The step thresholds are LandBenchmark's screening conventions, not published standards. A Phase-1 environmental records review is what identifies prior uses.
LiveLandsat 5/7/8/9 Collection-2 Level-21mo agoScreening-gradeSource

On the ground

The 8 checks a satellite can't settle. In a real report these are a saved checklist you tick off; the items are the same, and each names the source that answers it.

Not measured this run — and why

A LandBenchmark report never fills a gap with a guess. These signals could not be measured for this parcel; each states its reason.

  • drive timerequires an OpenRouteService key (ORS_API_KEY not configured)
  • flood sarradar flood detection is built but withheld: on a dry control parcel it reads wetter than a lakebed that actually flooded, because smooth bare soil scatters radar like open water. We will not publish a number we know is wrong. The optical flood signal above is unaffected
  • flood zonesource unreachable, or no data coverage at this location, this run
  • landslidethe NASA susceptibility service is currently unreachable — this signal ships as soon as the source is back online
  • storm surgecoastal screen — no data inland (not applicable) or the NOAA service was unavailable this run

What this report is — and what it isn't

LandBenchmark is an automated Phase-1 desk screen. Every signal here is measured from satellite imagery and public records, with its method and source shown. It is not an ASTM E1527 Phase I Environmental Site Assessment, not a survey, and not a flood determination — those require a licensed professional and, in some cases, physically being on the land.

No remote tool can sample your soil. Intrusive testing — borings, test pits, groundwater wells, and laboratory analysis for heavy metals, hydrocarbons, VOCs, or bacteria — is Phase-2 work, performed on site by licensed professionals. Where a signal below suggests it, we say so plainly rather than implying our screen settled the question.

Who to call about this parcel

Generated from the signals that flagged above — not a generic list.

  1. Geotechnical engineer

    Ask for soil plasticity testing and a foundation recommendation.

    Survey data indicates expansive (shrink-swell) soil, which cracks foundations. Foundation design depends on tested soil properties at your building site.

    Triggered by: Expansive-soil potential

  2. Environmental professional

    Ask for a Phase I Environmental Site Assessment (ASTM E1527), covering the nearby records and the parcel's own history.

    EPA-registered contamination records sit close to this parcel. Off-site contamination migrates through groundwater and soil vapour, and our screen covers neither leaking storage tanks nor anything ever done on the parcel itself.

    Triggered by: Environmental records nearby (EPA)

How the measurements are made: methodology & sources. How often they are right: the Accuracy Ledger. A report is an automated Phase-1 desk screen — not a survey, a flood determination, or a substitute for on-site inspection.