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
- Water937 measured · 1 context
- Climate9510 measured · 1 context
- Buildability8416 measured · 1 hard · 3 context
- Surroundings948 measured · 1 context
- Access833 measured · 1 context
- Hazard888 measured · 2 context
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
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
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
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
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
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
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
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.
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
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
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)
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
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
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
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
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
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
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
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
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.
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
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
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
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
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.
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
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
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
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
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
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
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
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
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)
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
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
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
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
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
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
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
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
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
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
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
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
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
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.
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
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'.
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.
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.
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.
Water availability / rights
Legal water rights determine whether you may actually use or draw water on the land.
WRI Aqueduct 4.0; rights = jurisdictionalSoil type / bearing
Soil texture and presumptive bearing capacity govern foundation type and cost — but need a geotech.
USDA SSURGO/gNATSGO (US); FAO HWSD, SoilGrids (Poggio 2021) global; IBC 2021 §1806.2Legal / deeded access & easements
Without a recorded easement, physical road proximity does not guarantee a legal right to enter.
County recorder / title co. — no open datasetZoning & permitted uses
Zoning dictates what you may legally build and do on the land.
National Zoning Atlas (hint, US partial)Deed restrictions / HOA / CC&Rs
Recorded covenants can restrict use far beyond public zoning.
No open datasetMineral & oil/gas rights
Severed mineral rights let others drill or mine beneath your surface.
BLM MLRS; USGS MRDS/USMIN (hint)Setbacks & building restrictions
Dimensional setbacks shrink the actual buildable envelope within the parcel.
National Zoning Atlas (hint); ordinanceTitle / liens / encumbrances
Liens and encumbrances on title can block or complicate a purchase.
No open dataset
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 time — requires an OpenRouteService key (ORS_API_KEY not configured)
- flood sar — radar 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 zone — source unreachable, or no data coverage at this location, this run
- landslide — the NASA susceptibility service is currently unreachable — this signal ships as soon as the source is back online
- storm surge — coastal 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.
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
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.