GeoMapSuite
Elevation & Topo7 min readUpdated 2026-09-19

How to Find the Elevation of an Address or Location (Above Sea Level)

A complete guide to finding the exact elevation above sea level for any home address or coordinate point using USGS LiDAR, Copernicus 30m DEMs, and GPS sensors.

ER
Elena Rostova
Senior GIS Analyst & Remote Sensing Specialist
Fact-checked & reviewed by Dr. Marcus Vance
Direct Answer (Quick Summary)

To find the exact elevation of an address or location above sea level, you can query high-resolution Digital Elevation Models (DEMs) derived from airborne LiDAR and satellite radar. In the United States, the USGS 3D Elevation Program (3DEP) provides 1-meter to 10-meter bare-earth models. Using the free GeoMap Suite Elevation Finder or "What is My Elevation" tool, you can search any street address, click anywhere on the topographic map, or use your device GPS to get instant elevation in both feet and meters.

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What is My Elevation Tool

Get your instant GPS elevation and look up the altitude above sea level for any address in feet and meters.

Find My Elevation
01

3 Reliable Ways to Find the Elevation of Any Location

Whether you are checking a property for flood risk, setting up an amateur radio antenna, planning a cycling route, or calibrating a home weather station, there are three primary methods to determine elevation above sea level:

1
Online Elevation Lookups (Digital Elevation Models): The fastest and most accurate method for specific street addresses. Web GIS tools query government LiDAR databases (such as the USGS 3DEP database) to return the precise bare-earth ground elevation for the parcel.
2
Topographic Contour Maps: Reading physical or digital USGS 7.5-minute quadrangle topographic maps. Elevation is determined by interpolating between brown contour lines (index and intermediate contours) and reference benchmark spot heights.
3
Mobile Device Sensors (Barometer + GPS): Modern smartphones combine satellite trilateration from GPS/GLONASS/Galileo constellations with built-in MEMS barometric pressure sensors to estimate altitude in real time.
02

Understanding Vertical Datums: Orthometric vs. Ellipsoidal Height

When people ask for their "elevation above sea level", geodesists must distinguish between two different height measurements:

Orthometric Height ($H$): Physical height above the Geoid (an equipotential gravitational surface that closely approximates mean sea level). This is the elevation printed on topographic maps and construction benchmarks (e.g., NAVD88 in the United States).
Ellipsoidal Height ($h$): Geometric distance above the smooth mathematical WGS84 Reference Ellipsoid. Raw GPS chips calculate ellipsoidal height natively.
Geoid Undulation ($N$): The difference between the geoid and the reference ellipsoid: h = H + N.

In North America, geoid height (N) varies between -20 meters to -40 meters. If a software tool does not convert raw GPS ellipsoidal height to orthometric height using a geoid model (like GEOID18 or EGM96), your reported elevation can be off by more than 100 feet!

Vertical Datum Distinction

GeoMap Suite automatically applies geoid undulation corrections to convert raw GPS satellite heights into true orthometric elevation above Mean Sea Level (NAVD88 / EGM96).

03

Digital Elevation Models: USGS 3DEP, SRTM, and Copernicus DEM

Modern elevation lookups rely on gridded raster elevation datasets known as Digital Elevation Models (DEMs):

USGS 3D Elevation Program (3DEP): The premier elevation dataset for the United States. Compiled from airborne LiDAR (Light Detection and Ranging) surveys, it offers bare-earth spatial resolutions of 1 meter (approx. 3.3 feet) and 1/3 arc-second (approx. 10 meters) with vertical accuracy within 5 to 15 centimeters.
Copernicus DEM (GLO-30): Produced by the European Space Agency from TanDEM-X satellite radar interferometry. It provides global coverage at 30-meter grid resolution and is widely regarded as the most uniform global elevation dataset.
NASA SRTM (Shuttle Radar Topography Mission): Flew aboard the Space Shuttle Endeavour in February 2000, mapping 80% of Earth's landmass at 1 arc-second (30m) resolution. Still used as a foundational baseline for global topography.
04

Why Smartphone Sensors Diverge From True Topographic Elevation

When you stand on your front porch and compare your iPhone or Android altitude reading with an official USGS survey marker, you will often notice a discrepancy of 15 to 50 feet. Why does this happen?

1
Satellite Geometry (Dilution of Precision): GPS satellites orbit high above the Earth. Because all visible satellites are above the horizon (none below your feet), vertical positioning geometry is inherently 2 to 3 times less accurate than horizontal latitude/longitude positioning.
2
Atmospheric Barometric Fluctuations: Built-in smartphone barometers estimate altitude by sensing air pressure. However, passing weather fronts, indoor heating/AC drafts, and seasonal temperature shifts alter ambient barometric pressure, causing uncalibrated altimeters to drift by 50+ feet over several hours.
3
Bare-Earth LiDAR Accuracy: In contrast, airborne LiDAR pulses pierce tree canopies and ground vegetation to measure the actual solid dirt surface, providing millimeter-calibrated elevation benchmarks.
05

Elevation Dataset Resolution & Vertical Accuracy Comparison

Here is how major elevation data sources compare in terms of spatial resolution, vertical accuracy, and ideal use cases:

Reference Data Table

Elevation Data Source Accuracy Matrix

Verified empirical measurements & benchmark coordinates

Data SourceSpatial ResolutionVertical AccuracyCoveragePrimary Technology
USGS 3DEP LiDAR (1m)1 meter (3.28 ft)±5 to 15 cm (0.2–0.5 ft)Contiguous USAirborne LiDAR Scanning
USGS 3DEP (10m)10 meters (1/3 arc-sec)±0.5 to 1.5 metersUnited States & TerritoriesLiDAR & Photogrammetry
Copernicus DEM (GLO-30)30 meters (1 arc-sec)±2 to 4 metersGlobal (Pole to Pole)Spaceborne Radar Interferometry
NASA SRTM (30m)30 meters (1 arc-sec)±5 to 9 metersGlobal (60°N to 56°S)C-band Radar Interferometry
Consumer Smartphone GPSN/A (Point Sensor)±5 to 15 meters (15–50 ft)Global Satellite Line-of-SightL1/L5 GNSS Trilateration
Smartphone BarometerN/A (Pressure Sensor)±1 to 3m (when calibrated)Ambient Air PressureMicro-Electro-Mechanical (MEMS)
06

Practical Reasons to Know Your Exact Property Elevation

Knowing your precise elevation above sea level is vital across numerous real-world scenarios:

FEMA Flood Zone & Insurance Determination: Determining if your home's lowest finished floor or mechanical equipment sits above the 100-year Base Flood Elevation (BFE).
High-Altitude Acclimatization: Travelers adjusting to elevation changes in mountainous destinations (such as Denver at 5,280 ft or Santa Fe at 7,199 ft).
Gardening & Plant Hardiness: Elevation directly affects local microclimates, frost dates, and temperature lapse rates (air cools approximately 3.5°F for every 1,000 feet of ascent).
Cooking & Baking Adjustments: Lower atmospheric pressure at higher elevations requires adjustments to boiling times, leavening agents, and oven temperatures.
Telecommunications & HAM Radio: Calculating line-of-sight propagation paths and Fresnel zone clearances for long-distance wireless links.
Interactive Calculators

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People Also Ask

People Also Ask About How to Find the Elevation of an Address or Location (Above Sea Level)

Essential questions answered with verified geodesic formulas, datum standards, and practical mapping advice.

Google Maps only displays elevation contour lines when viewing the map in "Terrain" mode, and it does not display numerical elevation for specific street addresses. To get the exact numeric elevation in feet or meters for a specific address, you must use a dedicated elevation tool like GeoMap Suite Elevation Finder.

Topics:#Elevation Finder#What is My Elevation#USGS 3DEP#LiDAR DEM#Sea Level Altitude#Topographic Contours
Editorial Standards & Verification
Authored by Elena Rostova

Senior GIS Analyst & Remote Sensing Specialist

Specializing in geodetic algorithms, WGS84 coordinate mathematics, and large-scale spatial mobility studies across North America and Europe.

Peer-Reviewed by Dr. Marcus Vance

Principal Cartographer

Reviewed against the calculation method and source limitations documented for each tool. Provider-backed results and real-world conditions can vary.

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