Agate Beach
Faces the big lake. Use the offshore wave record to see when the lake experienced stronger storm activity and how the waves changed afterward.
Burt Township beach information ↗See the storm peak, follow the waves as they ease or build again, and compare the open shoreline with the protected harbor. Built from real Lake Superior buoy measurements.
Actual open-lake waves north of Grand Marais, plus independently checked NWS marine warnings. This describes offshore conditions, not rock exposure or beach safety.
Measured offshore conditions only; no photographs needed.
Important: A reported wave decline is not proof of newly exposed rocks or safe access. The remote Marquette water-level gauge cannot certify Grand Marais beach exposure.
GRMM4 reports actual wind but no measured wave heights. Offshore waves are independently observed by GLOS SPOT-1361. Wind and wave directions can differ because of swell and fetch.
NOAA GRMM4 original station ↗ · A stronger or calmer measured wind is not a prediction of newly exposed stones or a beach safety clearance.
This is the timing of measured offshore waves, not a prediction of fresh agates, safe access or beach wave height.
No photographs required; source gaps cannot be treated as calm conditions.
This is an observed offshore activity comparison, not wave power or measured movement of agates at the beach. Photographs are not required.
This compares the buoy's latest complete 24-hour wave-activity measurement with its own 2026 June–October archive. A percentile is not the likelihood of finding agates or a safety rating.
The current Marquette reading above is separate. The following side-by-side comparison is an archived October 16, 2026 original-source example from two Lake Superior water-level sensors. Neither gauge measures actual shoreline height, water runup, or new stones at Agate Beach.
Checking original NOAA station/time provenance. This is not a current waterline reading at Grand Marais.
Why it matters: The lake can slosh after waves ease. A gauge reading hundreds of kilometers along the shore cannot tell us how many inches of pebble beach are exposed in Grand Marais. NOAA's Lake Superior seiche research ↗
Checking original Grand Marais Spotter observations. Gaps will not be filled.
Measured waves describe the open lake. The sheltered Bayshore Park harbor is not instrumented by this buoy.
We ran the photo-free environmental engine repeatedly across the original 2026 Grand Marais Spotter records. These figures describe how often sufficient buoy data were available—not whether stones appeared on the beach.
In this 2026 replay, three observation checkpoints showed renewed offshore waves; three had stale readings and one had a recent reporting gap. Those checks are not independent storms. Missing readings did not become calm-beach or safe-access claims.
Original-source walk-forward verification and tests. The replay did not use photos, pretend to know historic NWS warnings, validate gravel movement, or estimate odds of finding agates. Current lake conditions appear in the live observations above, not these dated percentages.
How high did the waves get? Did they ease off, or rise again? Explore the measured wave history that helps explain when Lake Superior has been active around Grand Marais.
Eight observed wave episodes between July and October 2026, grouped from original buoy readings.
Pick a measured episode to follow the lake's rise and recovery.
Wave observations are shown with their recorded UTC dates.
October 14 buoy waves traveled from roughly NNW, near the historical Agate Beach shoreline-facing direction.
Peak height isn't the whole story. This comparison uses observed wave height, mean period, direction and duration from the same Grand Marais buoy. It's not a chance of finding agates, a beach-wave prediction, or a safe-visit signal.
Only original buoy readings, with observation gaps excluded.
Relative to the strongest sufficiently sampled 2026 offshore episode only. The index integrates Hs² × recorded mean period over observed intervals of 90 minutes or less; it is not absolute wave power (kW/m), sediment transport, or agate exposure. The historical shoreline-facing direction is not a surveyed modern beach bearing.
Faces the big lake. Use the offshore wave record to see when the lake experienced stronger storm activity and how the waves changed afterward.
Burt Township beach information ↗Inside the Grand Marais harbor. Its protected setting makes local marine conditions and harbor-specific information especially useful to check.
Burt Township park information ↗Historical wave observations through October 14, 2026, not a live beach reading. Use the current forecast, posted access conditions and local collecting rules when planning a visit.
The simulated open-coast wave record shows recent disturbance followed by a sustained decline. A real result would still require verified shoreline exposure, hazards, and observations.
Illustrative candidate · not a visit recommendation72-hour example history and following 12-hour example forecast
The engine must clear each stage before showing an opportunity.
Documented public sites around Grand Marais. Location roles are evidence-based; the wave readouts above are simulations.
Burt Township identifies this as a public rockhounding beach and documents parking by the boardwalk. Open-lake exposure makes it the primary site for future storm research.
Township beach details ↗Public swimming beach inside Grand Marais harbor. Useful to demonstrate why the same offshore waves cannot automatically be assigned to a sheltered shoreline. Not an independently documented agate deposit.
Township park details ↗A simple orientation sketch, not a navigable map.
The live version must make uncertainty visible rather than hide it.
A closer source than East Superior: GLOS Seagull Grand Marais Spotter SPOT-1361, operated by Superior Watershed Partnership. These are real offshore observations, not beach surf or predicted exposed stones.
A new source-verified rolling archive retained 142 original readings from October 12–14, including one sustained elevated-wave episode (83 related measurements, not 83 separate storms). This offshore wave change is promising input for the future post-storm engine, not a validated collecting opportunity, a protected-harbor wave estimate, or a current shore hazard assessment.
GLOS Grand Marais Spotter original data ↗ · Original source verification ↗
Compare observed offshore wave activity using height, mean period, and sustained duration rather than just the tallest wave. No photographs needed. This ranks what the buoy measured—not agate discoveries or measured movement on the beach.
Checking source-stamped relative offshore wave observations…
What the numbers mean: We integrate actual observations of significant wave height squared × observed mean wave period × measured elapsed hours. The output is a relative wave-activity proxy, not calibrated wave power or beach sediment movement. Gaps larger than 90 minutes are not filled; sparse episodes are not ranked. The 2014 charted shore direction is not a surveyed current wave-exposure factor.
Why duration changes the ranking: The October 5 offshore peak reached 2.51 m, yet accumulated more measured wave activity over its episode than the October 12 event that peaked at 2.57 m. Neither result predicts exposed agates, safe access or protected Bayshore Park waves.
Original Grand Marais buoy ↗ · 5,291-reading calculation and tests ↗
Research-only wave history from 5,243 original Grand Marais Spotter readings across 111 UTC days, June 26 to October 14. These are open-lake measurements, not conditions at a collecting beach.
Interpretation: An episode means related elevated buoy readings, not a separate meteorological storm. A peak, falling wave height, or 48-hour observation record does not establish beach safety, shoreline changes or fresh agates.
Burt Township confirms both public waterfront destinations. That does not make both agate-producing beaches, allow rock removal, or establish safe post-storm conditions. This research gate keeps each claim separate.
Open Lake Superior shoreline
Township public beach and historic boardwalk; the Chamber describes the town's traditional rockhounding destination.
Sheltered Grand Marais harbor
Township swimming beach with bathhouse, parking and playground. Not an independently verified agate deposit.
Loading locally sourced pilot readiness audit. No current surf, collecting clearance or rock-exposure claim is made.
Research priority: A same-view beach photo from just before the July 21, 2026 observed offshore event. That event has an uncertain later photo date but no comparable earlier frame.
These are historical, noindex research disclosures. A shoreline or legal-collecting clearance will not appear until independently verified; no wave or photo status here is a current invitation to enter the water.
An event-by-event review of eight real Grand Marais offshore wave episodes. Photo dates come from independent sources; this panel does not estimate exposed stones, safe shoreline conditions, or visit windows.
Location trap: Another Agate Beach is near Toivola in Stanton Township. A July 2026 photo was explicitly identified there, not at Grand Marais. It is excluded from this evidence queue. Photos shot during a storm cannot be labeled “after.”
Evidence audit uses existing publicly dated images and the archived GLOS Grand Marais Spotter records. The weekly Wikimedia check uses one bounded metadata request and preserves newly discovered source details in a source-stamped photo review inbox, without additional visitor requests. Missing photos, unverified beach views and source-metadata revisions never create a fresh-agate or safety recommendation.
Local Grand Marais reporting gives us a critical reality check: Lake Superior waves and shore ice can uncover rocks, but they can also carry rocks away or bury them under sand. These are firsthand historical accounts—not a measured 2026 Agate Beach outcome.
A March 2012 Grand Marais area shoreline report describes shore ice bringing loose rocks up and leaving them as it melted. Conditions differed by beach segment.
In a November 2013 report, a longtime local rockhound documented stretches of formerly rocky shore with little exposed rock—including Woodland Park during August—after repeated storms.
A separate 2009–2014 spring-beach comparison shows that shore ice can also keep rocks inaccessible into late March in some years. Conclusion: Offshore waves alone tell us a disturbance happened—not whether the right pebbles will be exposed at Agate Beach. These historical observations have not been calibrated against the 2026 GLOS events.
Historical observer evidence is dated and geographically broader than the Agate Beach study point. No current beach condition, collecting window, or fresh-agate probability is inferred.
Independent dated photographs are the missing piece. We can now document a real Agate Beach scene and investigate a later report, but we cannot yet verify new stones were exposed by a particular storm.
Source-audit registry: independent photo metadata, exact GLOS July event timestamps, unreviewed OSM pilot geometry, and separate marine hazard controls. Loading local verification summary.
Why 10 m satellite images cannot resolve new pebbles ↗ · Why NAIP cannot capture every storm ↗
Two independently dated photographs show a broadly similar Grand Marais coastal landscape, twelve years apart. Similar-looking bluffs are not proof of a shared camera position. This visual is a candidate review, not a before-and-after storm result.
The same photographer also took a Grand Marais photo toward the open Lake Superior horizon around 10:36 on May 31, 2014, only six minutes after the coastal scene. That frame lacks the same bluffs and trees. Same date, photographer and named town do not mean the images share the same view.
Checking the local licensed-source comparison audit. No additional image matching or live-wave claims are supplied if it is unavailable.
Repeat-photo target, for future remotely sourced imagery: match the 2026 camera's position, identifiable bluffs/tree landmarks and view direction; verify both capture clocks, water level, lighting and wave runup. A historical landscape match cannot replace a storm-bracketing pair.
Original camera geotag, CC BY-SA 2.0. A dated earlier lake-coast photograph, not the same surveyed viewpoint. View original Wikimedia photo ↗
Original camera geotag, CC BY 4.0. Both sources have upload dates later than their original photo dates. View original Agate photo ↗
The source data were checked in October 2026. Neither photograph brackets a measured 2026 wave event from the same fixed camera location. Dated source ≠ documented exposed rocks.
Three dated wave episodes from NOAA buoy 45004 in eastern Lake Superior. These are actual observations—not simulated data and not waves measured at Agate Beach.
All data points were sampled from NOAA's archived East Superior station record.
Checking observation coverage.
NOAA buoy source ↗Historical source: NOAA NDBC THREDDS 45004h9999, significant wave height (meters), sampled approximately every 3 hours. Missing readings omitted and shown as gaps. Wave direction and local stone observations are not included in this dataset.
Actual NOAA charted geography checked against independent Great Lakes water/land mapping. These findings are not live surf or a rock-finding forecast.
Historic NOAA coastline tangent suggests a northwest-facing research shoreline. Six independent water/land tests agreed with the lakeward side.
2014 chart source · research bearing only, not a surveyed 2026 shoreline normal.NOAA charts two substantial harbor-entrance piers. A mapped pier does not tell us how much the waves diminish behind it.
Pier geometry dates to 2004–2014. NOAA soundings cover the harbor, but current depths, structure condition and wave attenuation remain unverified.Verified source coverage, not a live depth survey or harbor-wave forecast. These geographic areas overlap, so their record counts cannot be added together.
| Study area | Soundings | Depth contours |
|---|---|---|
| Inner southwest harbor | 17 | 6 |
| Harbor center | 41 | 12 |
| Entrance piers | 38 | 12 |
| Lake approach | 42 | 2 |
Underlying NOAA ENC sounding source dates: 2004–2020. The contour records provide no individual survey dates. Charts cannot establish current harbor depths, navigable clearance, wave shelter, or whether rocks have been exposed.
A recent USACE harbor survey record is now confirmed, while none of these sources establishes measured waves inside Grand Marais Harbor.
Decision-engine status: historic harbor structures documented; actual harbor wave heights, wave transmission, beach safety and new-stone exposure not verified. This prototype does not convert wind or survey dates into wave predictions.
Source: NOAA ENC Direct, checked against GLAHF mapped water. Neither beach has a validated wave or safety verdict.
Prototype only. Simulated wave scenarios are embedded in this page; the separate historical buoy chart loads dated NOAA observations. The shoreline summary is historic NOAA chart research, not live beach weather. No device location, personal data, account, tracking, or map key is needed.